鄂尔多斯盆地基底特征及西、南缘奥陶纪构造演化及沉积响应
|
摘要
鄂尔多斯盆地不仅油气资源丰富，也是我国钾盐找矿远景区。奥陶纪全球蒸发岩形成条件欠佳，但在鄂尔多斯盆地中东部的陕北地区依然沉积了巨厚的岩盐，并且达到了钾镁盐沉积阶段，说明鄂尔多斯盆地奥陶纪具备成盐成钾的古构造、古气候、古地理条件，但一些基础问题仍然悬而未决。本文对鄂尔多斯西、南缘十多条奥陶系剖面进行了详细观察和采样分析，并开展了岩石学、地层学、地球化学、沉积学、地球物理学以及锆石年代学等方面的研究，取得了如下认识：
1、通过对鄂尔多斯盆地及周缘高精度、大比例尺航磁异常资料ΔT化极、上延处理，获得了有关磁异常分区信息。航磁化极上延异常图上正、负异常分别与盆地结晶基底的隆起和凹陷大致吻合，表明基底埋深可能是航磁异常的基本控制因素。结合鄂尔多斯盆地基底断裂、基底变质岩与花岗岩锆石SHRIMPU-Pb定年、钻井和碎屑锆石年龄证据，认为鄂尔多斯陆块可能不是一个完整的太古宙陆块；
2、在贺兰山地区中奥陶统樱桃沟组首次发现内波、内潮汐沉积和等深流沉积；
3、对樱桃沟组碎屑岩进行了地球化学及岩石学分析，认为樱桃沟组物源区主要为主动大陆边缘，也有来自被动大陆边缘的信息。结合中奥陶世鄂尔多斯西缘古水流和碎屑锆石年龄分布特征，认为樱桃沟组的物源主要来自祁连造山带，部分来自阿拉善古陆；
4、获得了鄂尔多斯盆地西南缘陕西泾阳西陵沟剖面和甘肃平凉银洞官庄剖面奥陶系平凉组钾质斑脱岩的地球化学特征和锆石U-Pb年龄。地球化学特征表明样品的钾质特征，以及其原始岩浆为高钾亚碱性流纹英安岩和粗面安山岩，多数样品具有典型的岛弧火山岩的特征。通过LA-ICP-MS锆石U-Pb定年，获得了6组谐和年龄。根据钾质斑脱岩区域分布判断其源于南部北秦岭地区或/和西南部北祁连地区的火山喷发。综合分析表明，平凉组多层钾质斑脱岩代表的构造活动期代表了秦岭-祁连洋向北俯冲最强烈的时期，并直接导致了鄂尔多斯盆地南缘奥陶系重大沉积转换。
There is growing concern about the Ordos Basin because of its hydrocarbon resources. It should be noted, though, that the Ordos basin is also potash ore prospect areas in China. In the geological background of global poor evaporite deposits, huge rock salt deposited in North Shaanxi Province, located in the central and eastern Ordos Basin, and it achieved the depositional phase of potassium and magnesium salt. These indicate there are paleotectonics, paleoclimate, paleogeographic conditions for potassium salt in the Ordos Basin. Some basic geological problems, however, remain controversial. On the basis of references to the predecessors' researches, this paper did detailed observation and sampling analysis of field sections in the southern and western margin of the Ordos Basin and conducted the studies of lithology, stratigraphy, geochemistry, sedimentology, geophysics and zircon chronology. Obtained as follows:
1. Aeromagnetic anomaly zonation of the Ordos Basin and adjacent areas was obtained by processing high-precision and large-scale aeromagnetic anomalies with an approach of reduction to the pole upward continuation. Basement depth might be the fundamental control factor for aeromagnetic anomalies because the positive and negative anomalies on the reduction to the pole-upward-continuation anomaly maps roughly coincide with the uplifts and depressions of the crystal-line basement in the basin. The results, together with the latest understanding of basement faults, SHRIMP U-Pb zircon dating of metamorphic rock and granite, drilling data, detrital zircon ages, and gravity data interpretation, suggest that the Ordos block is not an entirety of Archean.
2. This paper firstly discovered internal-wave, internal-tide deposits and contourite in the Middle Ordovician Yingtaogou Formation in the Helan Mountain area.
3. The petrologic and geochemical characteristics of sandstone from Yingtaogou Formation have been researched systematically. The geochemical signatures indicate its double provenance supply feature. After comprehensive consideration of the middle Ordovician palaeocurrents in the western Ordos and detrital zircon age features, we suggest that the provenance of Yingtaogou Formation was mainly the North qilian orogenic belt and the Alashan paleolandmass as a minor one.
4. We report the geochemical and zircon U-Pb dating on K-bentonite samples collected from two sections, located in Jingyang County, Shaanxi Province and Pingliang City, Gansu Province. The major elements and the Nb-Zr diagram show the potassium-rich characteristic. Inactive elements in the process of weathering are employed to reconstruct the protolith, and the result demonstates primary magma of the K-bentonites is high-potassium alkaline rhyolitic dacite and trachyandesite. Most of the K-bentonite samples show typical characteristics of arc volcanic rocks, which were probably related to the subduction setting. LA-ICP-MS U-Pb dating on zircons from4K-bentonites samples in Xilinggou profile and2samples from Yindongguanzhuang profile has yielded6sets of concordant ages. Accordingly, the main depositional period of Pingliang Formation, which is still controversial, is redefined to Sandbian-Katian, Late Ordovician. According to their regional distribution, it is thought that these K-bentonites derive from volcanic eruption in the southern North Qinling or/and southwestern North Qilian region. Composite analysis indicates that the important sedimentary turn appearing the south Ordos Basin results from the subduction northward of Qinling-Qilian ocean. Volcanic eruption events represented by these K-bentonites beds have a good coupling relationship with periodic subsidence and filling process of North Qinling back-arc basin (southern margin of Ordos basin).
1、通过对鄂尔多斯盆地及周缘高精度、大比例尺航磁异常资料ΔT化极、上延处理，获得了有关磁异常分区信息。航磁化极上延异常图上正、负异常分别与盆地结晶基底的隆起和凹陷大致吻合，表明基底埋深可能是航磁异常的基本控制因素。结合鄂尔多斯盆地基底断裂、基底变质岩与花岗岩锆石SHRIMPU-Pb定年、钻井和碎屑锆石年龄证据，认为鄂尔多斯陆块可能不是一个完整的太古宙陆块；
2、在贺兰山地区中奥陶统樱桃沟组首次发现内波、内潮汐沉积和等深流沉积；
3、对樱桃沟组碎屑岩进行了地球化学及岩石学分析，认为樱桃沟组物源区主要为主动大陆边缘，也有来自被动大陆边缘的信息。结合中奥陶世鄂尔多斯西缘古水流和碎屑锆石年龄分布特征，认为樱桃沟组的物源主要来自祁连造山带，部分来自阿拉善古陆；
4、获得了鄂尔多斯盆地西南缘陕西泾阳西陵沟剖面和甘肃平凉银洞官庄剖面奥陶系平凉组钾质斑脱岩的地球化学特征和锆石U-Pb年龄。地球化学特征表明样品的钾质特征，以及其原始岩浆为高钾亚碱性流纹英安岩和粗面安山岩，多数样品具有典型的岛弧火山岩的特征。通过LA-ICP-MS锆石U-Pb定年，获得了6组谐和年龄。根据钾质斑脱岩区域分布判断其源于南部北秦岭地区或/和西南部北祁连地区的火山喷发。综合分析表明，平凉组多层钾质斑脱岩代表的构造活动期代表了秦岭-祁连洋向北俯冲最强烈的时期，并直接导致了鄂尔多斯盆地南缘奥陶系重大沉积转换。
There is growing concern about the Ordos Basin because of its hydrocarbon resources. It should be noted, though, that the Ordos basin is also potash ore prospect areas in China. In the geological background of global poor evaporite deposits, huge rock salt deposited in North Shaanxi Province, located in the central and eastern Ordos Basin, and it achieved the depositional phase of potassium and magnesium salt. These indicate there are paleotectonics, paleoclimate, paleogeographic conditions for potassium salt in the Ordos Basin. Some basic geological problems, however, remain controversial. On the basis of references to the predecessors' researches, this paper did detailed observation and sampling analysis of field sections in the southern and western margin of the Ordos Basin and conducted the studies of lithology, stratigraphy, geochemistry, sedimentology, geophysics and zircon chronology. Obtained as follows:
1. Aeromagnetic anomaly zonation of the Ordos Basin and adjacent areas was obtained by processing high-precision and large-scale aeromagnetic anomalies with an approach of reduction to the pole upward continuation. Basement depth might be the fundamental control factor for aeromagnetic anomalies because the positive and negative anomalies on the reduction to the pole-upward-continuation anomaly maps roughly coincide with the uplifts and depressions of the crystal-line basement in the basin. The results, together with the latest understanding of basement faults, SHRIMP U-Pb zircon dating of metamorphic rock and granite, drilling data, detrital zircon ages, and gravity data interpretation, suggest that the Ordos block is not an entirety of Archean.
2. This paper firstly discovered internal-wave, internal-tide deposits and contourite in the Middle Ordovician Yingtaogou Formation in the Helan Mountain area.
3. The petrologic and geochemical characteristics of sandstone from Yingtaogou Formation have been researched systematically. The geochemical signatures indicate its double provenance supply feature. After comprehensive consideration of the middle Ordovician palaeocurrents in the western Ordos and detrital zircon age features, we suggest that the provenance of Yingtaogou Formation was mainly the North qilian orogenic belt and the Alashan paleolandmass as a minor one.
4. We report the geochemical and zircon U-Pb dating on K-bentonite samples collected from two sections, located in Jingyang County, Shaanxi Province and Pingliang City, Gansu Province. The major elements and the Nb-Zr diagram show the potassium-rich characteristic. Inactive elements in the process of weathering are employed to reconstruct the protolith, and the result demonstates primary magma of the K-bentonites is high-potassium alkaline rhyolitic dacite and trachyandesite. Most of the K-bentonite samples show typical characteristics of arc volcanic rocks, which were probably related to the subduction setting. LA-ICP-MS U-Pb dating on zircons from4K-bentonites samples in Xilinggou profile and2samples from Yindongguanzhuang profile has yielded6sets of concordant ages. Accordingly, the main depositional period of Pingliang Formation, which is still controversial, is redefined to Sandbian-Katian, Late Ordovician. According to their regional distribution, it is thought that these K-bentonites derive from volcanic eruption in the southern North Qinling or/and southwestern North Qilian region. Composite analysis indicates that the important sedimentary turn appearing the south Ordos Basin results from the subduction northward of Qinling-Qilian ocean. Volcanic eruption events represented by these K-bentonites beds have a good coupling relationship with periodic subsidence and filling process of North Qinling back-arc basin (southern margin of Ordos basin).
引文
An M J, Feng M, Zhao Y. Destruction of lithosphere within the North China Craton inferred from surface wave tomography. Geochemistry Geophysics Geosystems,2009,10, Q08016, doi:10.1029/2009GC002562
Anderson T. Correction of common lead in U-Pb analyses that do not report204Pb. Chemical Geology,2002,192:59-79
Badenas B, Pomar L, Aurell M et al. A facies model for internalites (internal wave deposits) on a gently sloping carbonate ramp (Upper Jurassic, Ricla, NE Spain). Sedimentary Geology,2012,271-272:44-57
Bahadur R A M, Singh N P, Murthy A S K. Aeromagnetic Anomalies Uncover the Precambrian Basement in the Chhattisgarh Basin Area, Central India. Acta Geophysica,2008,56:982-993
Bergstrom S M, Huff W D, Kolata D R. The Lower Silurian Osmundsberg K-bentonite. Part I: stratigraphic position, distribution, and palaeogeographic significance. Geological Magazine,1997,135:1-13
Bhatia M R, Crook K A. Trace Element Characteristics of Graywackes and Tectonic Setting Discrimination of Sedimentary Basins. Contributions to Mineralogy and Petrology,1986,90(2):181-193
Bhatia M R, Taylor S R. Trace-element Geochemistry and Sedimentary Provinces:a Study from the Tasman Geosyncline, Australia. Chemical Geology,1981,33(1/2):115-125
Bhatia M R. Plate Tectonics and Geochemical Composition of Sandstones. The Journal of Geology,1983,91(6):611-627
Bhatia M R. Rare Earth Element Geochemistry of Australian Paleozoic Graywackes and Mudrocks:Provenance and Tectonic Control. Sedimentary Geology,1985,45(1/2):97-113.
Boynton W V. Cosmochemistry of the rare earth elements:Meteorite studies. Dev Geochem,1984,2:63-114
Calarge L M, Meunier A, Formoso ML L. A bentonite bed in the Acegua (RS, Brazil) and Melo (Uruguay) areas:a highly crystallized montmorillonite. Journal of South American Earth Scienees,2003,16:187-198
Carlson R W, Pearson D G, James D E. Physical, Chemical, and chronological characteristics of continental mantle. Reviews of Geophysics,2005,43, RG1001, doi:10,1029/2004RG000156
Carroll A R, Grahamwand S A, Smith M E. Walledsedimentary basinsof China, BasinResearch,2010,22:17-32
Chen L. Lithospheric structure variations between the eastern and central North China Craton from S-and P-receiver function migration. Physics of the Earth and Planetary Interiors2009,173:216-227
Chen L, Cheng C, Wei Z G. Seismic evidence for significant lateral variations in lithospheric thickness beneath the central and western North China Craton. Earth and Planetary Science Letters,2009a,286:171-183
Chen L, Sun Y, Diwu C R, Wang H L. Crust for mation in the Ordos block:Constraints from detrital zircons from Ordovican and Permian sandstones. In:Abstract with Program of International Discussion meeting on Continental Geology and Tectonics. Northwest University Press, Xi'an,2009b.17
Chen L, Wang T, Zhao L, et al. Distinct lateral variation of lithospheric thickness in the Northeastern North China Craton. Earth and Planetary Science Letters2008,267:56-68
Chen L, Zheng T Y, Xu W W. A thinned lithospheric image of the Tanlu Fault Zone, eastern China: Constructed from wave equation based receiver function migration. Journal of Geophysical Research2006,111:B09312,doi:10.1029/2005JB003974
Cheng C, Chen L, Yao H J, et al. Distinct variations of crustal shear wave velocity structure and radial anisotropy beneath the North China Craton and tectonic implications. Gondwana Research,2013,23:25-38
Compston W. Interpretations of SHRIMP and isotope dilution zircon ages for the geological time-scale:1. The early Ordovician and late Cambrian. Mineralogical Magazine,2000,64(1):43-57
Condie K C. Another look at rare earth elements in shales. Geochimica et Cosmochimica Acta,1991,55:2527-2531
Darby B J, Gehrels G E. Detrital zircon reference for the North China block. Journal of Asian Earth Sciences,2006,26:637-648
Darby B J, Ritts B D. Mesozoic contractional deformation in the middle of the asian tectonic collage; the intraplate western Ordos Fold-Thrust Belt, China. Earth and Planetary Science Letters2002,205:13-24
Desmares D, Grosheny D, Beaudoin B, et al. High resolution stratigraphic record constrained by volcanic ash beds at the Cenomanian-Turonian boundary in the Western Interior basin, USA. Cretaceous Research,2007,28:561-582
Dickinson W R, Gehrels G E. U-Pb ages of detrital zircons in Jurassic eolian and associated sandstones of the Colorado Plateau:Evidence for transcontinental dispersal and intraregional recycling of sediment. Geological Society of America Bulletin,2009,121:408-433
Dickinson W R, Suczek C A. Plate tectonics and sandstone compositions. The American Association of Petroleum Geologists Bulletin,1997,63(12):2164-2182
Dickinson W R. Interpreting provenance relations from detrital modes of sandstones. In:Zuffa G G ed. Provenance of Arenites. Dordrecht:D. Reidel, NA TO-ASI Series1985,148:333-361
Dickinson W R. Provenance of North American Phanerozoic sandstones in relation to tectonic setting. GSA Bulletin,1983,94:222-235
Diwu C R, Sun Y, Zhang H, et al. Episodic tectonothermal events of the western North China Craton and North Qinling Orogenic Belt in central China:Constraints from detrital zircon U-Pb ages. Journal of Asian Earth Sciences2012,47:107-122
Dohan K, Sutherland B R. Numerical and laboratory generation of internal waves from turbulence. Dynamics of Atmospheres and Oceans,2005,40:43-56
Dong H L, Hall C M, Halliday A N, et al.40Ar/39Ar illite dating of Late Caledonian(Acadian) metamorphism and cooling of K-bentonites and slate from the Welsh basin, UK. Earth and Planetary Science Letters,1997,150:337-351
Du Y, Wang J, Han X, et al. From flysch to molasse-the sedimentary and tectonic evolution of the late Caledonian-early Hercynian foreland basin in North Qilian Mountains. Journal of China University of Geosciences,2003,13(1):1-7
Du L L, Yang C H, Wang W, et al. Paleoproterozoic rifting of the North China Craton: Geochemical and zircon Hf isotopic evidence from the2137Ma Huangjinshan A-type granite porphyry in the Wutai area. Journal of Asian Earth Sciences2013,72:190-202
Enkelmann E, Weislogel A, Ratschbacher L, et al. How was the Triassic Songpan-Ganzi Basin filled? A provenance study. Tectonics,2007,26, TC4007:1-24
Fang L F, Wu J P, Ding Z F, et al. Crustal velocity structures beneath North China revealed by ambient noise tomography. Earthquake Science2010,23:477-486
Faure M, Lin W, Monie P, Bruguier O. Palaeoproterozoic arc magmatism and collision in Liaodong Peninsula (northeast China). Terra Nova2004,16:75-80
Faure M, Trap P, Lin W, Monie P, Bruguier O. Polyorogenic evolution of the Paleoproterozoic Trans-North China Belt, new insights from the Luliangshan-Hengshan-Wutaishan and Fuping massifs. Episodes2007,30:1-12
Fleet A R. Aqueous and sedimentary geochemistry of the rare earth elements. In:Henderson P.(ed.),Rare Earth Element Geochemistry, Elsevier,1984:331-373
Foreman B Z, Rogers R R, Deino A L, et al. Geochemical characterization of bentonite beds in the two Medicine Formation (Campanian, Montana), in eluding a new40Ar/39Ar age. Cretaceous Research,2007, doi:10.1016/j.cretres2007.07.001
Gao Z Z, Eriksson K A, He Youbin, et al. Deep-Water Traction Current Deposits-A Study of Internal Tides, Internal Waves, Contour Currents and Their Deposits. Beijing and New York: Science Press, Utrecht and Tokyo:VSP,1998
Gao Z Z, Eriksson K A. Internal-tide deposits in an Ordovician submarine channel:Previously unrecognized facies?. Geology,1991,19(7):734-737
Gao Z Z, He Y B, Li J M, et al. The first internal-tide deposits found in China. Chinese Science Bulletin,1997,42(13):1113-1117
Gehrels G E, Yin A, Wang X F. Detrital zircon geochronology of the northeastern Tibetan Plateau. Geological Society of America Bulletin,2003,115:881-896
Gerkema T, Lam F P A, Maas L R M. Internal tides in the Bay of Biscay:conversion rates and seasonal effects. Deep-Sea Research Ⅱ,2004,51(25/26):2995-3008
Gerkema T, Staquet C, Bouruet Aubertot P. Nonlinear effects in internal-tide beams, and mixing. Ocean Modelling,2006,12:302-318
Girty G H, Hanson A D, Knaack C, et al. Provenance Determined by REE, Th, and Sc Analyses of Metasedimentary Rocks, Boyden Cave Roof Pendant, Central Sierra Nevada, California. Journal of Sedimentary Research,1994,64(1):68-73
Gradstein F M, Ogg J G and Smith A G. A Geologic Time Scale. Camdridge:Cambridge University Press,2004.1-589
Guo J H, Peng P, Chen Y, et al. UHT sapphirine granulite metamorphism at1.93-1.92Ga caused by gabbronorite intrusions:implications for tectonic evolution of the northern margin of the North China Craton. Precambrian Research,2012, doi.org/10.1016/j. precamres.2011.07.020
Guo J H, Sun M, Chen F K, et al. Sm\Nd and SHRIMP U\Pb zircon geochronology of high-pressure granulites in the Sanggan area, North China Craton:timing of Paleoproterozoic continental collision. Journal of Asian Earth Sciences,2005,24:629-642
Haughton P D, Todd S P, Morton AC. Sedimentary provenance studies. Geological Society, London, Special Publications.1991,57:1-11
Haynes J T, Melson W G, Kunk M J. Composition of biotite phenocrysts in Ordovician tephras casts doubt on the proposed trans. Atlantic correlation of the Millbrig K-bentonite (United States) and the Kinnekulle K-bentonite (Sweden). Geology,1995,23(9):847-850
He Y B, Luo J X, Gao Z Z, et al. Reply to the Discussion of He et al.(2011, Geo-Marine Letters) Evidence of internal-wave and internal-tide deposits in the Middle Ordovician Xujiajuan Formation of the Xiangshan Group, Ningxia, China. Geo-Marine Letters,2012,32:367-372
He Y B, Luo J X, Li X D, et al. Evidence of internal-wave and internal-tide deposits in the Middle Ordovician Xujiajuan Formation of the Xiangshan Group, Ningxia, China. Geo-Marine Letters,2011,31:509-523
He Y B, Gao Z Z. The Characteristics and recognition of internal-tide and internal-wave deposits. Chinese Science Bulletin,1999,44(7):582-589
Helge J H, Harald F, Ole J M. Paleogene tuffaceous intervals, Grane Field(Block25-11), Norwegian North Sea:their depositional, petrographical, geochemical character and regional implications. Marine and Petroleum Geology,2000,17:101-118
Hendrix M S. Evolution of Mesozoic sandstone compositions, Southern Junggar, Northern Tarim, and Western Turpan Basins, Northwest China:A detrital record of the ancestral Tian Shan. Journal of Sedimentary Research,2000,70(3):520-532
Hu Y H, Zhou J B, Song B, et al. SHRIMP zircon U-Pb dating from K-bentonite in the top of Ordovician of Wangjiawan Section, Yichang, Hubei, Science China (D),2008,51(4):493-498
Hu J M, Liu X S, Li Z H, et al.. SHRIMP U-Pb zircon dating of the Ordos Basin basement and its tectonic significance. Chinese Science Bulletin2012,57, doi:10.1007/s11434-012-5274-0
Huang X L, Zhong J W, Xu Y G. Two tales of the continental lithospheric mantle prior to the destruction of the North China Craton:Insights from Early Cretaceous mafic intrusions in western Shandong, East China. Geochimica et Cosmochimica Acta,2012,96:193-214
Huertas M O, Palomo I,Moresi M,et al. A mineralogical and geochemical approach to establish a sedimentary model in a passive continental margin Sabbetic Zone, Betic Cordilleras, Sepein. Clay Minerals,1991,26:389-407
Huff W D, Bergstrom S M, Kolata D R, et al. The Lower Silurian Osmundsberg K-bentonite. Part Ⅱ:mineralogy, geochemistry, chemo stratigraphy and tectonomagmatic significance. Geological Magazine,1997b,135:15-26
Huff W D, Bergstrom S M, Kolata D R. Gigantic Ordovician volcanic ash fall in North Amerrica and Europe:Biological, tectonomagmatic, and event-stratigraphic significance. Geology,1992,20:875-878
Huff W D, Bergstrom S M, Kolata D R. Silurian K-bentonites of the Dnestr Basin, Podolia, Ukraine. Journal of the Geological Society,2000,157:493-504
Huff W D. Ordovician K-bentonites:Issues in interpreting and correlating ancient tephras. Quaternary International,2008,178:276-287
Huff W D, Bergstrm S M, Kolata D R. Gigantic Ordovician volcanic ash fall in North America and Europe:Biological, tectonomagmatic, and event-stratigraphic significance. Geology,1992,20(10):875-878
Jackson S E, Pearson N J, Griffin W L, et al. The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U-Pb zircon geochronology. Chemical Geology,2004,211:47-69
Jia C Z, Li B L, Zhang X Y, et al. Formation and evolution of the Chinese marine basins. Chinese Science Bulletin,2007,52:1-11
Jian P, Liu D Y, Kroner A, et al. Time scale of an Early to Mid-Paleozoic orogenic cycle of the long-lived Central Asian Orogenic Belt, Inner Mongolia of China:implications for continental growth. Lithos,2008,101:233-259
Johnson A C, Swain C J. Further evidence of fracture-zone induced tectonic segmentation of the Antarctic Peninsula from detailed aeromagnetic anomalies. Geophysical Research Letters1995,22:1917-1920
Kolata D R, Huff W D, Bergstrom S M. Nature and regional significance of unconformities associated with the Middle Ordovician Hagan K-bentonite complex in the North American midcontinent. Geological Society of America Bulletin,1998,110:723-739
Kroner A, Wilde S A, Li J H, et al. Age and evolution of a late Archaean to early Palaeozoic upper to lower crustal section in the Wutaishan/Hengshan/Fuping terrain of northern China. Journal of Asian Earth Sciences2005a,24:577-595
Kroner A, Wilde S A, O'Brien P J, et al. Feild relationships, geochemistry, zircon ages and evolution of a late Archean to Paleoproterozoic lower crustal section in the Hengshan Terrain of Northern China. Acta Geologica Sinica (English Edition)2005b,79:605-629
Kroner A, Wilde S A, Zhao G C, et al. Zircon geochronology of mafic dykes in the Hengshan Complex of northern China:evidence for late Palaeoproterozoic rifting and subsequent high-pressure event in the North China Craton. Precambrian Research2006,146:45-67
Kusky T M. Geophysical and geological tests of tectonic models of the North China Craton. Gondwana Research2011a,20:26-35
Kusky T M. Comparison of results of recent seismic profiles with tectonic models of the North China craton. Journal of Earth Sciences2011b,22:250-259
Kusky T M, Li J H. Paleoproterozoic tectonic evolution of the North China Craton. Journal of Asian Earth Sciences2003,22:383-397
Kusky T M., Li J H, Santosh M. The Paleoproterozoic North Hebei Orogen:North China Craton's collisional suturewith the Columbia supercontinent. Gondwana Research2007,12:4-28
Kusky T M, Santosh M. The Columbia connection in North China. In:Reddy, S.M., Mazumder, R., Evans, D., Collins, A.S.(Eds.), Paleoproterozoic Supercontinents and Global Evolution Geological Society of London, Special Publication,2009,323:49-71
Kusky T M, Li J H, Tucker R D. The Archean Dongwanziophiolitecomplex, North ChinaCraton:2.505billion year old oceanic crust andmantle. Science2001,292:1142-1145
Lan T G, Fan H R, Hu F F, et al. Multiple crust-mantle interactions for the destruction of the North China Craton:Geochemical and Sr-Nd-Pb-Hf isotopic evidence from the Longbaoshan alkaline complex. Lithos2011,122:87-106
Li S G, Huang F, Nie Y H, et al. Geochemical and geochronological constraints on the suture location between the North and South China blocks in the Dabie orogen, central China. Physics and Chemistry of the Earth,2001,26:655-672
Li H K, Lu S N, Su W B, et al. Recent advances in the study of the Mesoproterozoic geochronology in the North China Craton. Journal of Asian Earth Sciences2013a,72:216-227
Li H Y. Destruction of North China Craton:Insights from temporal and spatial evolution of the proto-basins and magmatism. Science China Earth Sciences,2013,56(3):464-478
Li H Y, Xu Y G, Liu Y M, et al. Detrital zircons reveal no Jurassic plateau in the eastern North China Craton. Gondwana Research2013b,24:622-634
Li J W, Bi S J, Selby D, et al. Giant Mesozoic gold provinces related to the destruction of the North China craton. Earth and Planetary Science Letters,2012a,349-350:26-37
Li M, Gao J R. Basement faults and volcanic rock distributions in the Ordos Basin. Science China: Earth Sciences,2010, doi:10.1007/s11430-010-4042-8
Li S Z, Zhao G C, Dai L N, et al. Cenozoic faulting of the Bohai Bay Basin and its bearing on the destruction of the eastern North China Craton. Journal of Asian Earth Sciences,2012b,47:80-93
Li X P, Yang Z Y, Zhao G C, et al. Geochronology of khondalite-series rocks of the Jining Complex:confirmation of depositional age and tectonometamorphic evolution of the North China craton. International Geology Review,2011,53:1194-1211
Li, Z W, Hao T Y, Xu Y. Uppermost mantle structure of the North China Craton:Constraints from interstation Pn travel time difference tomography. Chinese Science Bulletin2011,56, doi:10.1007/s11434011-4487-y
Lin W, Wang Q C, Wang J, et al. Late Mesozoic extensional tectonics of the Liaodong Peninsula massif:Response of crust to continental lithosphere destruction of the North China Craton. SCIENCE CHINA Earth Sciences,2011,54:843-857
Ling M X, Li Y, Ding X, et al. Destruction of the North China Craton Induced by Ridge Subductions. Journal of Geology,2013,121(2):197-213
Liu Y S, Gao S, Hu Z C, et al. Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen:U-Pb dating, Hf isotopes and trace elements in zircons from mantle xenoliths. Journal of Petrology,2009,51:537-571
Lv B, Zhai M G, Li T S, et al. Zircon U\Pb ages and geochemistry of the Qinglong volcano～sedimentary rock series in Eastern Hebei:implication for～2500Ma intra～continental rifting in the North China Craton. Precambrian Research,2012,208-211:145-160
Lu Y F, Xu M J, Wang L S, et al. Crustal structure of the southeastern margin of the OrdosBlock. Chinese Science Bulletin2011,56:3854-3859, doi:10.1007/s11434-011-4847-7
Ludwig K R. User's manual for Isoplot/Ex, version3.00. A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center Special Publication,2003,4:1-70
Mao J W, Zhang Z C, Zhang Z H, et al. Re-Os isotopic dating of molybdenites in Xiaoliugou W(Mo) deposit in the northern Qilian mountains and its geological significance. Geochemical et Cosmochemica Acta,1999,63:1815-1818
Mao J W, Zhang Z H, Jian P, et al. U-Pb zircon dating of the Yeniutan granitic intrusion in the western sector of the North Qilian Mountains. Acta Geologica Sinica,2000,74:781-785
Marker P G, Huff W D. What is a K-bentonite? Geological Society of America Abstracts with Programs,2005,37:143
McLennan S M. Rare earth elements in sedimentary rocks:influence of provenance and sedimentary processes. In:Lipin B R and McKay G A (eds). Geochemistry and mineralogy of rare earth elements. Mineralogical Society of America,1989,21:169-200
Najman Y. The detrital record of orogenesis:A review of approachs and techniques used in the Himalayan sedimentary basins. Earth-Science Reviews,2006,74:1-72
Pearce J A, Harris N B W, Tindle A G. Trace element discrimination diagrams for the tectonic
interpretation of granitic rocks. Journal of Petrology,1984,25:956-983
Pearce J A, Norry M J. Petrogenetic implications of Ti, Zr, Y, and Nb variations in volcanic rocks. Contributions to Mineralogy and Petrology,1979,69:33-47
Pei F P, Xu W L, Yang D B, et al. Geochronology and geochemistry of Mesozoic mafic-ultramafic complexes in the southern Liaoning and southern Jilin provinces, NE China:Constraints on the spatial extent of destruction of the North China Craton. Journal of Asian Earth Sciences, 2011,40:636-650
Peng P, Guo J H, Windley B F, et al. Halaqin volcano-sedimentary succession in the central-northern margin of the North China Craton:products of Late Paleoproterozoic ridge subduction. Precambrian Research,2011,187:165-180
Peng T P, Fan W M, Peng P X. Geochronology and geochemistry of late Archean adakitic plutons from the Taishan granite-greenstone Terrain:implications for tec-tonic evolution of the eastern North China Craton. Precambrian Research,2012,208-211:53-71
Pomar L, Morsilli M, Hallock P, et al. Internal waves, an under-explored source of turbulence events in the sedimentary record. Earth-Science Reviews,2012,111:56-81
Pomar L, Morsilli M, Hallock P, et al. Reply to Shanmugam, G., comment on "Internal waves, an underexplored source of turbulence events in the sedimentary record" by Pomar et al.[Earth-Science Reviews,111(2012),56-81], Earth Science Reviews (2012). Earth-Science Reviews,2013,116:206-210
Ram B, Singh N P, Murthy A S K. A note on the qualitative appraisal of aeromagnetic image of Chhattisgarh basin. Journal of Indian Geophysical Union,2007,11:129-133
Ray R D, Mitchum G T. Surface manifestation of internal tides in the deep ocean:observations from altimetry and island gauges. Progression of Oceanography,1997,40:135-162
Ren L D, Geng Y S, Du L L, et al. SHRIMP data on zircons from the Wanzi series:Constraints on the rock formation time and implications of migmatization at2.1-2.0Ga in the Fuping Complex, North China Craton. Journal of Asian Earth Sciences,2013,72:203-215
Ribbe J, Holloway P E. A model of suspended sediment transport by internal tides. Continental Shelf Research,2001,21:395-422
Roser B P, Korsch R J. Determination of Tectonic Setting of Sandstone-mudstone Suites Using SiO2Content and K20/Na2O Ratio. The Journal of Geology,1986,94(5):635-650
Santosh M. Assembling North China Craton within the Columbia superconti～nent:the role of double-sided subduction. Precambrian Research,2010,178:149-167
Santosh M, Kusky T M. Origin of paired high pressure-ultrahigh-temperature orogens:a ridge subduction and slab window model. Terra Nova,2010,22:35-42
Santosh M, Liu S J, Tsunogae T, et al. Paleoproterozoic ultrahigh-temperature granulites in the North China Craton:implications for tectonic models on extreme crustal metamorphism. Precambrian Research,2012. http://dx.doi.org/10.1016/j.precamres.2011.05.003
Santosh M, Sajeev K, Li J H. Extreme crustal metamorphism during Columbia supercontinent assembly:evidence from North China Craton. Gondwana Research2006,10:256-266
Santosh M, Sajeev K, Li J H, et al. Counterclockwise exhumation of a hot orogen:the Paleoproterozoic ultrahigh-temperature granulites in the North China Craton. Lithos,2009a,110:140-152
Santosh M, Tsunogae T, Li J H. Discovery of sapphirine-bearing Mg-Al granulites in the North China Craton:implications for Paleoproterozoic ultrahigh temperature metamorphism. Gondwana Research,2007a,11:263-285
Santosh M, Tsunogae T, Ohyama H, et al. Carbonic meta-morphism at ultrahigh-temperatures: evidence from North China Craton. Earth and Planetary Science Letters,2008,266:149-165.
Santosh M, Wan Y, Liu D, et al. Anatomy of zircons from an ultrahot Orogen:the amalgamation of North China Craton within the supercontinent Columbia. Journal of Geology,2009a,117:429-443
Santosh M, Wilde S A, Li J H. Timing of Paleoproterozoic ultrahigh temperature metamorphism in the North China Craton:evidence from SHRIMP U-Pb zircon geochronology. Precambrian Research,2007b,159:178-196
Santosh M, Zhao D P, Kusky T M. Mantle dynamics of the Paleoproterozoic North China Craton: a perspective based on seismic tomography. Journal of Geodynamics2010,49:39-53
Shanmugam G. Discussion of He et al.(2011, Geo-Marine Letters) Evidence of internal-wave and internal-tide deposits in the Middle Ordovician Xujiajuan Formation of the Xiangshan Group, Ningxia, China. Geo-Marine Letters,2012,32:359-366
Shanmugam G. Modern internal waves and internal tides along oceanic pycnoclines:Challenges and implications for ancient deep-marine baroclinic sands. AAPG Bulletin,2013b,97(5):799-843
Shanmugam G. New perspectives on deep-water sandstones:Implications. Petroleum Exploration and Development,2013a,40(3):316-324
Shen J F, Santosh M, Li S R, et al. The Beiminghe skarn iron deposit, eastern China: Geochronology, isotope geochemistry and implications for the destruction of the North China Craton. Lithos,2013,156-159:218-229
Shi Y, Yu J H, Santosh M. Tectonic evolution of the Qinling orogenic belt, Central China:New evidence from geochemical, zircon U-Pb geochronology and Hf isotopes. Precambrian Research,2013,231:19-60
Song S G, Niu Y, Zhang L F, et al. Tectonic evolution of early Paleozoic HP metamorphic rocks in the North Qilian Mountains, NW China:new perspectives. Journal of Asian Earth Sciences.2009,35:334-353
Song S G, Niu Y L, Su L, et al. Tectonics of the North Qilian orogen, NW China. Gondwana Research,2013,23:1378-1401
Su W B, He L Q, Wang Y B, et al. K-bentonite beds and high-resolution integrated stratigraphy of the uppermost Ordovician Wufeng and the lowest Silurian Longmaxi formations in South China. SCIENCE CHINA:Earth Sciences,2003,46:1121-1133
Su W B, Huff W D, Frank R E, et al. K-bentonite, black shale and flysch successions at the Ordovician-Silurian transition, South China:Possible sedimentary responses to the accretion of Cathaysia to the Yangtze Block and its implications for the evolution of Gondwana. Gondwana Research,2009, doi:10.1016/j.gr.2008.06.004
Su W B, Li H K, Huff W D, et al. SHRIMP U-Pb dating for a K-bentonite bed in the Tieling Formation, North China. Chinese Science Bulletin,2010,55:3312-3323
Su W B, Zhang S H, Huff W D, et al. SHRMP U-Pb ages K-bentuonite beds in the Xiamaling Formation:Implications for revised subdivision of the Meso-to Neoproterozoic history of the North China Craton. Gondwana Research,2008, doi:10.101b/j.gr.2008.04.007
Sun W D, Li S G, Sun Y, et al. Mid-paleozoic collision in the north Qinling:Sm-Nd, Rb-Sr and40Ar/39Ar ages and their tectonic implications. Jounal of Asian Earth Sciences,2002,21:69-76
Sun Z, Xie Q, and Yang J. Ordos basin-A typical example of an unstable cratonic interior superimposed basin, in X. Zhu and W. Xu, eds., Chinese sedimentary basins:Amsterdam, Elsevier,1989.148-168
Sutherland B R, Hughes G O, Dalziel S B, et al. Internal waves revisited. Dynamics of Atmospheres and Oceans,2000,31:209-232
Taylor S R, Mclennan S M. The continental crust:its composition and evolution:An examination of the geochemical record preserved in sedimentary rocks. Oxford:Blackwell Scientific Publications,1985
Tian Y, Zhao D P. Destruction mechanism of the North China Craton:Insight from P and S wave mantle tomography. Journal of Asian Earth Sciences,2011,42:1132-1145
Tian Y, Zhao D P, Sun R M, et al. Seismic imaging of the crust and upper mantle beneath the North China Craton. Physics of the Earth and Planetary Interiors,2009,172:169-182
Tseng C Y, Yang H J, Yang H Y, et al. Continuity of the North Qilian and North Qinling orogenic belts, Central Orogenic System of China:Evidence from newly discovered Paleozoic adakitic rocks. Gondwana Research,2009,16:285-293
Wan Y S, Dong C Y, Liu D Y, et al. Zircon ages and geochemistry of late Neoarchean syenogranites in the North China Craton:A review. Precambrian Research,2012. http://dx.doi.org/10.1016/j.precamres.2011.05.001
Wan Y S, Liu D Y, Wang S J, et al.2.7Ga juvenile crust formation in the North China Craton (Taishan-Xintai area, western Shandong Province):Further evidence of an understated event from U-Pb dating and Hf isotopic composition of zircon. Precambrian Research,2011,186:169-180
Wang C Y, Zhang Q, Qian Q, et al. Geochemistry of the early Paleozoic Baiyin volcanic rocks (NW China):implications for the tectonic evolution of the North Qilian orogenic belt. The Journal of Geology.2005,113:83-94
Wang C, Jin Z M, Gao S, et al. Eclogite melt/peridotite reaction:Experimental constrains on the destruction mechanism of the North China Craton. SCIENCE CHINA Earth Sciences,2010,53:797-809
Wang F, Li X P, Chu H, Zhao G C. Petrology and metamorphism of khondalites from Jining Complex in the North China Craton. International Geology Review,2011,53:212-229
Wang H Z, Mo X X. An outline of the tectonic evolution of China. Episodes,1996:6-16
Wang S Y, Xu Z H, Pei S P. Velocity structure of uppermost mantle beneath China continent from Pn tomography. Science China:Earth Sciences,2002,45:143-150
Wang T, Guo L, Zheng Y D, et al. Timing and processes of late Mesozoic mid-lower-crustal extension in continental NE Asia and implications for the tectonic setting of the destruction of the North China Craton:Mainly constrained by zircon U-Pb ages from metamorphic core complexes. Lithos,2012,154:315-345
Wang X X, Wang T, Zhang C L. Neoproterozoic, Paleozoic, and Mesozoic granitoid magmatism in the Qinling Orogen, China:Constraints on orogenic process. Journal of Asian Earth Sciences,2013,72:129-151
Wilde S A, Cawood P A, Wang KY, et al. Granitoid evolution in the late Archean Wutai Complex, North China Craton. Journal of Asian Earth Sciences,2005,24:597-613
Wilde S A, Valley J W, Kita N T, et al. SHRIMP U-Pb and CAMECA1280oxygen isotope results from ancient detrital zircons in the Caozhuang quartzite, Eastern Hebei, North China Craton: evidence for crustal reworking3.8Ga ago. American Journal of Science,2008,308:185-199
Wilde S A, Zhao G C. Archean to Paleoproterozoic evolution of the North China Craton. Journal of Asian Earth Sciences,2005,24:519-522
Wilde S A, Zhao G C, Sun M. Development of the North China Craton during the Late Archaean and itsfinal amalgamation at1.8Ga; some speculations on its position within a global Palaeoproterozoic supercontinent. Gondwana Research,2002,5:85-94
Wilde S A, Zhao G C, Wang K Y, et al. First precise SHRIMP U-Pb zircon ages for the Hutuo Group, Wutaishan:further evidence for the Palaeoproterozoic amalgamation of the North China Craton. Chinese Science Bulletin,2004,49:83-90
Winchester J A, Floyd P A. Geochemical discrimination of different magma series and their differentiation products using immobile elements. Chemical Geology,1977,20:325-343
Winn R D. Large-scale traction produced structures in deep-water fan-channel conglomerates in southern chile. Geology,1977,5:41-44
Wu C L, Shi R D, Yang J S, et al. Petrogenesis and dating of two types of granite from North Qilian, China. Acta Geologica Sinica,2005,79:193-200
Wu Q F, Lu F X, Liu Q S, et al. Archean relic body at lower crust in Sulu area:Evidence from magnetic data. Chinese Science Bulletin,2003,48:589-593
Wynn R B, Stow D A V. Recognition and inter pretation of deep-water sediment waves: implications for palaeoceanography, hydrocarbon exploration and flow process in terpretation. Marine Geology,2002,192:1-3
Xia L Q, Xia Z C, Xu X Y. Magmagenesis in the Ordovician backarc basins of the North Qilian Mountains, China. GSA Bulletin,2003,115:1510-1522
Xia Q, Liu J, Liu S, et al. High water content in the Mesozoic lithospheric mantle of the North China Craton and implications for its destruction. Earth and Planetary Science Letters,2013,361:85-97
Xia X P, Sun M, Zhao G C, et al. LA-ICP-MS U-Pb geochronology of detrital zircons from the Jining Complex, North China Craton and its tectonic significance. Precambrian Research,2006b,144:199-212
Xia X P, Sun M, Zhao G C, et al. U-Pb and Hf isotopic study of detrital zircons from the Wulashan khondalites:Constraints on the evolution of the Ordos Terrane, Western Block of the North China Craton. Earth and Planetary Science Letters,2006a,241:581-593
Xia, X.P., Sun, M., Zhao, G.C., Wu, F.Y., Xu, P., Zhang, J.S. Paleoproterozoic crustal growth events in the Western Block of the North China Craton:Evidence from detrital zircon Hf and whole rock Sr-Nd isotopes of the khondalites in the Jining Complex. American Journal of Science,2008,308:304-327
Xie X Y, Heller P L. U-Pb detrital zircon geochronology and its implications:The early Late Triassic Yanchang Formation, south Ordos Basin, China. Journal of Asian Earth Sciences,2013,64:86-98
Xiong X L, Liu X C, Zhu Z M, et al. Adakitic rocks and destruction of the North China Craton: Evidence from experimental petrology and geochemistry. SCIENCE CHINA Earth Sciences,2011,54:858-870
Xu Y. Thermo-tectonic destruction of the Archaean lithospheric keel beneath the Sino-Korean Craton in China:Evidence, timing and mechanism. Phys Chem Earth,2001,26:747-757
Xu Y G, Li H Y, Pang C J, et al. On the timing and duration of the destruction of the North China Craton. Chinese Science Bulletin,2009,54, doi:10.1007/s11434-009-0346-5
Xue F, Kroner A, Reischmann T, et al. Palaeozoic pre-and post-collision calcalkaline magmatism in the Qinling orogenic belt, central China, as documented by zircon ages on granitoid rocks. Journal of the Geological Society,1996,153:409-417
Yang Y T, Li W, Ma L. Tectonic and stratigraphic controls of hydrocarbon systems in the Ordos Basin:a multicycle cratonic basin in central China. AAPG Bulletin,2005,89:255-269
Yang C H, Du L L, Ren L D, et al. Delineation of the ca.2.7Ga TTG gneisses in the Zanhuang Complex, North China Craton and its geological implications. Journal of Asian Earth Sciences,2013,72:178-189
Yang J H, Wu F Y, Wilde S A, et al. Mesozoic decratonization of the North China Block. Geology,2008,36:467-470
Yang Y T, Li W, Ma, L. Tectonic and stratigraphic controls of hydrocarbon systems in the Ordos basin:A multicycle cratonic basin in central China. AAPG Bulletin,2005,89:255-269
Yin C Q, Zhao G C, Guo J H, et al. U-Pb and Hf isotopic study of zircons of the Helanshan Complex:constrains on the evolution of the Khondalite Belt in the Western Block of the North China Craton. Lithos2011,122:25-38
Yin C Q, Zhao G C, Sun M, et al. LA-ICP-MS U-Pb zircon ages of the Qianlishan Complex: constrains on the evolution of the Khondalite Belt in the Western Block of the North China Craton. Precambrian Research,2009,174:78-94
Yuan W, Yang Z. The Alashan Terrane was not part of North China by the Late Devonian: Evidence from detrital zircon U-Pb geochronology and Hf isotopes, Gondwana Research,2014, http://dx.doi.Org/10.1016/j.gr.2013.12.009
Zeng H L, Xu D S, Tan H D. A model study for estimating optimum upward-continuation height for gravity separation with application to a Bouguer gravity anomaly over a mineral deposit, Jilin province, northeast China. Geophysics,2007,72(4):145-150
Zhai M G. Multi-stage crustal growth and cratonization of the North China Craton, Geoscience Frontiers,2014, doi:10.1016/j.gsf.2014.01.003
Zhai MG, Liu W J. Paleoproterozoic tentonic history of the North China Craton:A review. Precambrian Research,2003,122:183-199
Zhai M G, Bian A G, Zhao T P. The amalgamation of the supercontinent of North China Craton at the end of Neo～Archaean and its breakup during late Palaeoproterozoic and Mesoproterozoic. Science in China (Series D-Earth Science),2000,43:219-232
Zhai M G, Guo J H, Liu W J. Neoarchean to Paleoproterozoic continental evolution and tectonic history of the North China craton. Journal of Asian Earth Sciences,2005,24:547-561
Zhai M G, Liu W J. An oblique cross-section of Precambrian crust in the North China Craton. Physics and Chemistry of Earth (A),2001,26:781-792
Zhai M G, Santosh M. The early Precambrian odyssey of North China Craton:a synoptic overview. Gondwana Research,2011,20:6-25
Zhai M G, Shao JA, Hao J, et al. Geological signature and possible position of the North China block in the Supercontinent Rodinia. Gondwana Research,2003,6:171-183
Zhang C H, Li C M, Deng H L, et al. Mesozoic contraction deformation in the Yanshan and northern Taihang mountains and its implications to the destruction of the North China Craton. SCIENCE CHINA Earth Sciences,2011,54:798-822
Zhang C L, Liu L, Wang S J, et al. Detrital zircon provenance for the meta-sedimentary rocks from Kuanping Group, implicati on for Neo-proerozoic tectonic reconstruction in Qinling Orogeny, central China. In:Abstract with program of international discussion meeting on continental geology and tectonics. Northwest University Press, Xi'an,2009.64-66
Zhang H F. Destruction of ancient lower crust through magma underplating beneath Jiaodong Peninsula, North China Craton:U-Pb and Hf isotopic evidence from granulite xenoliths. Gondwana Research,2012a,21:281-292
Zhang H F, Sun M, Zhou X H, et al. Mesozoic lithosphere destruction beneath the North China Craton:Evidence from major, trace element and Sr-Nd-Pb isotope studies of Fangcheng basalts. Contributions to Mineralogy and Petrology,2002,144:241-254
Zhang H F, Ying J F, Santosh M, et al. Episodic growth of Precambrian lower crust beneath the North China Craton:A synthesis. Precambrian Research,2012a,222-223:255-264
Zhang H F, Zhu R X, Santosh M, et al. Episodic widespread magma underplating beneath the North China Craton in the Phanerozoic:Implications for craton destruction. Gondwana Research,2012b, doi:10.1016/j.gr.2011.1012.1006
Zhang J, Li J Y and Liu J F. Detrital zircon U-Pb ages of Early Paleozoic flysch sandstones in the western Ordos margin-New constrains on their provenances and rentonic implications. Journal of Asian Earth Sciences,2011,42:1030-1047
Zhang J F, Wang C, Wang Y F. Experimental constraints on the destruction mechanism of the North China Craton. Lithos,2012b,149:91-99
Zhang K J. Destruction of the North China Craton:Lithosphere folding-induced removal of lithospheric mantle? Journal of Geodynamics,2012b,53:8-17
Zhang Y B, Zhai M G, Lin Q, et al. Late Cretaceous volcanic rocks and associated granites in Gyeongsang Basin, SE Korea:Their chronological ages and tectonic implications for cratonic destruction of the North China Craton. Journal of Asian Earth Sciences,2012c,47:252-264
Zhao G C. Paleoproterozoic assembly of the North China Craton. Geology Magazine,2001,138:87-91
Zhao G C, Cawood P A. Precambrian Geology of China. Precambrian Research,2012,222-223:13-54
Zhao G C, Cawood P A, Wilde S A, et al. Metamorphism of basement rocks in the Central Zone of the North China Craton:implications for Paleoproterozoic tectonic evolution. Precambrian Research,2002,103:55-88
Zhao G C, Cawood P A, Wilde S A, et al. Amalgamation of the North China Craton:key issues and discussion. Precambrian Research,2012,222-223:55-76
Zhao G C, Kroner A, Wilde S A, et al. Lithotectonic elements and geological events in the Hengshan-Wutai-Fuping belt:a synthesis and implications for the evolution of the Trans-North China Orogen. Geological Magazine,2007,144:753-775
Zhao G C, Sun M, Wilde S A, et al. Late Archean to Paleoproterozoic evolution of the North China Craton:key issues revisited. Precambrian Research,2005,136:177-202
Zhao G C, Wilde S A, Cawood P A, et al. Thermal evolution of two textural types of mafic granulites in the North China Craton:evidence for both mantle plume and collisional tectonics. Geology Magazine,1999a,136:223-240
Zhao G C, Wilde S A, Cawood P A, et al. Tectonothermal history of the basement rocks in the western zone of the North China Craton and its tectonic implications. Tectonophysics1999b,310:37-53
Zhao G C, Wilde S A, Cawood P A, et al. Petrology and P-T-t path of the Fuping mafic granulites: implications for tectonic evolution of the central zone of the North China Craton. Journal of Metamorphic Petrology,2000,18:375-391
Zhao G C, Wilde S A, Cawood P A, et al. Archean blocks and their boundaries in the North China Craton:lithological, geochemical, structural and P-T path constraints and tectonic evolution. Precambrian Research,2001a,107:45-73
Zhao G C, Wilde S A, Cawood P A, et al. High-pressure granulites (retrograded eclogites) from the Hengshan Complex, North China Craton:petrology and tectonic implications. Journal of Petrology,2001b,42:1141-1170
Zhao G C, Wilde S A, Cawood P A, et al. Thermal evolution of basement rocks from the eastern part of the North China Craton and its bearing on tectonic setting. International Geology Reviews,1998,40:706-721
Zhao G C, Wilde S A, Zhang J. New evidence from seismic imaging for subduction during assembly of the North China craton:COMMENT. Geology,2010,38:206
Zhao G C, Zhai M G. Lithotectonic elements of Precambrian basement in the North China Craton: Review and tectonic implications. Gondwana Research,2013,23:1207-1240
Zheng J P, Griffin W L, Ma Q, et al. Accretion and reworking beneath the North China Craton. Lithos,2012,149:61-78
Zheng T Y, Zhao L, Zhu R X. New evidence from seismic imaging for subduction during assembly of the North China Craton. Geology,2009,37:395-398
Zheng Y F, Xiao W J, Zhao G C. Introduction to tectonics of China. Gondwana Research,2013,23:1189-1206
Zhou L H, Fu L X, Lou D, et al. Structural anatomy and dynamics of evolution of the Qikou Sag, Bohai Bay Basin:Implications for the destruction of North China craton. Journal of Asian Earth Sciences,2012,47:94-106
Zhu R X, Chen L, Wu F Y, et al. Timing, scale and mechanism ofthe destruction of the North China Craton. SCIENCE CHINA Earth Sciences,2011,54:789-797
Zhu Z Y, Jiang S Y, Liu G X, et al. Precise dating of the Middle Permian:Zircon U-Pb geochronology from volcanic ash beds in the basal Gufeng Formation, Yangtze region, South China. Gondwana Research,2013,23:1599-1606
Zhu G, Jiang D Z, Zhang B L, et al. Destruction of the eastern North China Craton in a backarc setting:Evidence from crustal deformation kinematics. Gondwana Research,2012a,22:86-103
Zhu R X, Xu Y G, Zhu G, et al. Destruction of the North China Craton. SCIENCE CHINA Earth Sciences,2012, doi:10.1007/s11430-012-4516-y
Zhu R X, Zheng T Y. Destruction geodynamics of the North China Craton and its Paleoproterozoic plate tectonics. Chinese Science Bulletin,2009,54, doi:10.1007/s11434-009-0451-5
安太庠,郑昭昌.鄂尔多斯盆地周缘的牙形石.北京：科学出版社,1990：12-132
柏冠军,吴汉宁,赵希刚,等.重力资料识别鄂尔多斯盆地线性构造方法研究.地球物理学进展,2007,22(5)：1386-1392
白斌,周立发,张义楷,等.贺兰山深部构造及其对浅部构造的响应过程.大地构造与成矿学,2008,32(1)：42-49
白瑾,黄学光,王惠初,等.中国前寒武纪地壳演化(第二版).北京：地质出版社,1996
白云来,王新民,刘化清,等.鄂尔多斯盆地西部边界的确定及其地球动力学背景.地质学报,2006,80(6)：792-813
包洪平,杨承运.鄂尔多斯东部奥陶系马家沟组微相分析.古地理学报,2000,2(1)：31-42
鲍志东,李儒峰,冯增昭.鄂尔多斯盆地东西部奥陶系对比再研究.地质论评,1999,45(4):375~381
蔡忠贤,蔡华,秦玉娟.鄂尔多斯盆地南缘早古生代碳酸盐岩高频沉积旋回分析.地球科学,1997,22(5):504~510
曹金舟,冯乔,赵伟,等.鄂尔多斯盆地南缘奥陶纪层序地层分析.沉积学报,2011,29:286~292
车自成,罗金海,刘良.中国及其邻区区域大地构造学(第二版).北京:科学出版社,2011.19~23,238~256
陈安清.鄂尔多斯地块早古生代盆地演化与物质聚集规律.博士学位论文.成都:成都理工大学,2010.1~137
陈诚,史晓颖,裴云鹏,等.鄂尔多斯盆地南缘晚奥陶世钾质斑脱岩SHRIMP测年及其成因环境.现代地质,2012,26(2):205~219
陈化奇.北祁连冷龙岭地区宁缠河花岗岩体的地球化学特征及大地构造意义.甘肃地质,2007,16:37~42
陈九辉,刘启元,李顺成等.青藏高原东北缘~鄂尔多斯地块地壳上地幔S波速度结构.地球物理学报,2005,48(2):333~342
陈凌,程骋,危自根.华北克拉通边界带区域深部结构的特征差异性及其构造意义.地球科学进展,2010,25(6):571~581
陈凌,危自根,程骋.从华北克拉通中、西部结构的区域差异性探讨克拉通破坏.地学前缘,2010,1:212~228
陈孟晋,汪泽成,郭彦如,等.鄂尔多斯盆地南部晚古生代沉积特征与天然气勘探潜力.石油勘探与开发,2006,33(1):1~5
陈明远.鄂尔多斯盆地北部地区重力资料的解释方法及其效果.石油与天然气地质,1988,9(4):325~333
陈孟晋,宁宁,胡国艺,等.鄂尔多斯盆地西部平凉组烃源岩特征及其影响因素.科学通报,2007,52(增刊Ⅰ):78~85
陈强,张慧元,李文厚,等.鄂尔多斯奥陶系碳酸盐岩碳氧同位素特征及其意义.古地理学报,2012,14(1):117~124
陈荣坤,孟祥化.华北地台早古生代沉积建造及台地演化.岩相古地理,1993,13(4):46~55.
传婷婷.鄂尔多斯盆地西缘奥陶系沉积特征及构造意义.硕士学位论文.北京:中国地质大学(北京),2013.1~65
崔智林,华洪,宋庆原.晚奥陶世北秦岭弧后盆地放射虫组合.地质学报,2000,74:254~259
邸领军,谢广成.对贺兰拗拉槽的质疑.岩性油气藏,2008,20(2):16~21,36
丁海军,孟祥化,葛铭,等.贺兰拗拉谷北段奥陶系等深流沉积.地球科学与环境学报,2009,31(1):58~65
丁海军,孟祥化,葛铭.米钵山组复理石中的内潮汐沉积.安徽地质,2008,18(4):241~247
丁燕云.鄂尔多斯盆地北部航磁反映的构造特征.物探与化探.2000,24(3):197~203
邓晋福,吴宗絮,赵国春,等.华北地台前寒武纪花岗岩类、陆壳演化与克拉通形成.岩石学报,1999,15:190~198
邓军,王庆飞,黄定华,等.鄂尔多斯盆地基底演化及其对盖层控制作用.地学前缘,2005,12(3):91~99
董春艳,万渝生,徐仲元,等.华北克拉通大青山地区古元古代晚期孔兹岩系:锆石SHRIMPU-Pb定年.中国科学:地球科学,2012,42:1851~1862
董兆雄,姚泾利,孙六一,等.重新认识鄂尔多斯南部早奥陶世马家沟期碳酸盐台地沉积模式.中国地质,2010,37(5):1327~335
董兆雄,赵敬松,方少仙,等.鄂尔多斯盆地南部奥陶纪末端变陡缓坡沉积模式.西南石油学院学报,2002,24:50~53
杜远生,朱杰,韩欣,等.从弧后盆地到前陆盆地~北祁连造山带奥陶纪~泥盆纪的沉积盆地与构造演化.地质通报,2004,23(9~10):911~917
杜远生,颜佳新,韩欣.造山带沉积地质学研究的新进展.地质科技情报,1995,14(1):29~34
杜远生,朱杰,顾松竹,等.北祁连造山带寒武系~奥陶系硅质岩沉积地球化学特征及其对多岛洋的启示.中国科学:地球科学,2007,37(10):1314~1329
方迎尧,张培琴,刘浩军.低磁纬度地区ΔT异常解释的途径与方法.物探与化探,2006,30(1):48
费安玮,刘成林,甘军,等.鄂尔多斯盆地三道坎组混合沉积的生物扰动构造与古地理.中国地质,2004,31(4):347~355
费安玮,张忠涛.陕西金粟山中奥陶统生物扰动构造与古环境分析.地球科学,2002,27(6):703~710
冯益民,何世平.祁连山及其邻区大地构造基本特征~兼论早古生代海相火山岩的成因环境.西北地质科学,1995,16:92~103
冯益民,何世平.祁连山大地构造与造山作用.北京:地质出版社,1996:1~135.
冯增昭,鲍志东,康祺发,等.鄂尔多斯早古生代古地理.1999b,1,84~91
冯增昭,鲍志东,康祺法,等.鄂尔多斯早古生代古构造.古地理学报,1999,1(2):84~91.
冯增昭,鲍志东,张永生.鄂尔多斯奥陶纪地层岩石岩相古地理.北京:地质出版社,1998.1~144
冯增昭,鲍志东.鄂尔多斯奥陶纪马家沟期岩相古地理.沉积学报,1999a,17,1~8
付金华,郑聪斌.鄂尔多斯盆地奥陶纪华北海和祁连海演变及岩相古地理特征.古地理学报,2001,3(4):25~34
高振中,何幼斌,李向东.中国地层记录中的内波及内潮汐沉积研究.古地理学报,2010,12(5):527~534
高振中,何幼斌,刘成鑫,等.深水牵引流沉积的研究历程、现状与前景.古地理学报,2006,8(3):331~338
高振中,何幼斌,罗顺社,等著.深水牵引流沉积~内潮汐、内波和等深流沉积研究.北京:科学出版社,1996,1~112
高振中,何幼斌,张兴阳,等.塔中地区中晚奥陶世内波、内潮汐沉积.沉积学报,2000,18(3):400~407
高振中,罗顺社,何幼斌,等.鄂尔多斯地区西缘中奥陶世等深流沉积.沉积学报,1995b,13(4):16~26
高振中,罗顺社,何幼斌,等.鄂尔多斯西缘奥陶纪海底扇沉积体系.石油与天然气地质,1995a,16(2):119~126
葛梅钰,郑昭昌,李玉珍.宁夏及其邻近地区奥陶纪、志留纪笔石地层及笔石群.南京:南京大学出版社,1990,1~190
葛文春,吴福元,周长勇,等.大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约.科学通报,2005,50:1239~1247
耿建珍,张健,李怀坤,等.10μm尺度锆石U~Pb年龄的LA~MC~ICP~MS测定.地球学报,2012,33:877~884
耿元生,沈其韩,任留东.华北克拉通晚太古代末~古元古代初的岩浆事件及构造热体制.岩石学报,2010,26:1945~1966
管志宁,安玉林,吴朝钧.磁性界面反演及华北地区深部构造的推断.见:王懋基,程家印主编.
勘查地球物理勘查地球化学文集(第6集),中国区域地球物理研究.北京:地质出版社.1987,802~101
郭慧丽,徐佩芬.地震层析成像在华北克拉通地区的研究进展.地球物理学进展,2011,26(5):1557~1565
郭飚,刘启元,陈九辉,等.青藏高原东北缘~鄂尔多斯地壳上地幔地震层析成像研究.地球物理学报,2004,47(5):790~797
郭峰,郭岭,赵卫卫.贺兰坳拉谷奥陶纪岩相古地理．海相地质与第四纪地质,2011,31(5):51~58
郭锋,范蔚茗,李超文,等.早古生代古亚洲洋俯冲作用:来自内蒙古大石寨玄武岩的年代学与地球化学证据.中国科学D辑:地球科学,2009,39:569~579
郭建秋,张雄华,章泽军.江西修水地区中元古界双桥山群修水组内波内潮汐沉积.地质科技情报,2003,22(1):47~52
郭建秋,张雄华,章泽军,等.赣西北前寒武系首次发现内波内潮汐沉积.地质科学,2004,39(3):329~338
郭彦如,赵振宇,付金华,等.鄂尔多斯盆地奥陶纪层序岩相古地理.石油学报,2012,33(增刊2):95~109
郭依群,王嘹亮,匡增桂,等.等深流沉积特征.海洋地质前沿,2012,28(6):1~9
韩品龙,张月巧,冯乔.鄂尔多斯盆地祁连海域奥陶纪岩相古地理特征及演化.现代地质,2009,22:822~827
何幼斌,高振中,郭成贤,等.石门杨家坪下寒武统杷榔组三段内波和内潮汐沉积研究.中国地质,2005,32(1):62~69
何幼斌,高振中,李建明,等.浙江桐庐晚奥陶世内潮汐沉积.沉积学报,1998,16(1):1~7
何幼斌,高振中,张兴阳,等.塔里木盆地塔中32井中上奥陶统内潮汐沉积.古地理学报,2003,5(4):414~425
何幼斌,罗顺社,高振中.内波、内潮汐沉积研究现状与进展.江汉石油学院学报,2004,26(1):5~11
何幼斌,高振中,罗顺社,等.陕西陇县地区平凉组三段发现内潮汐沉积.石油天然气学报,2007,29(4):28~33
何自新,杨华,袁效奇.鄂尔多斯盆地地质剖面图集.北京:石油工业出版社,2004.1~422
何自新.鄂尔多斯盆地演化与油气.北京:石油工业出版社,2003:22~31
侯方浩,方少仙,赵敬松；等.鄂尔多斯盆地中奥陶统马家沟组沉积环境模式.海相油气地质,2002,7(1):38~46
侯方浩,方少仙,董兆雄,等.鄂尔多斯盆地中奥陶统马家沟组沉积环境与岩相发育特征.沉积学报,2003,21:106~112
胡波,翟明国,彭澎,等.华北克拉通古元古代末~新元古代地质事件-来自北京西山地区寒武系和侏罗系碎屑锆石LA~ICP~MSU~Pb年代学的证据.岩石学报,2013,29:2508~2536
胡波,翟明国,郭敬辉,等.华北克拉通北缘化德群中碎屑锆石的LA-ICP-MSU-Pb年龄及其构造意义.岩石学报,2009,25(1):193~211
胡晓,许传诗,牛树根.华北地台北缘早古生代大陆边缘演化.北京:北京大学出版社,1990,1~185
胡艳华,刘健,周明忠,等.奥陶纪和志留纪钾质斑脱岩研究评述.地球化学,2009,38,393~404
黄汲清.中国大地构造特征的新研究.中国地质科学院院报,1984,9:5~20
黄汲清等.中国大地构造及其演化.北京:科学出版社,1980
黄汲清,任纪舜,姜春发,等.中国大地构造基本轮廓.地质学报,1977,52(2):117~135黄喜峰,钱壮志,逯东霞,等.贺兰山中南段奥陶系米钵山组的沉积环境与构造背景分析.地球学报,2009,30(1):65~71
黄喜峰,钱壮志,孙保平,等.北祁连造山带与贺兰冷裂谷构造边界的探讨.桂林理工大学学报,2010,30(2):195~201
嵇少丞,王茜,许志琴.华北克拉通破坏与岩石圈减薄.地质学报,2008,82(2):174~193
贾进斗,何国琦,李茂松,等.鄂尔多斯盆地基底结构特征及其对古生界天然气的控制.高校地质学报,1997,3(2):144~153
嘉世旭,张先康.华北不同构造块体地壳结构及其对比研究.地球物理学报,2005,48:611~620
贾振远,蔡华,蔡忠贤,等．鄂尔多斯地区南缘奥陶纪层序地层及海平面变化．地球科学~中国地质大学学报,1997,22:491~503
贾振远.一个碳酸盐沉积古斜坡的基本特征.石油与天然气地质,1988,9:171~178
江为为,郝天珧,宋海斌.鄂尔多斯盆地地质地球物理场特征与地壳结构.地球物理学进展,2000,15(3):45~53
晋慧娟,李育慈,方国庆.西秦岭古代地层记录中内波、内潮汐沉积及其成因解释.沉积学报,2002,20(1):80~84
晋慧娟,李育慈,方国庆.中国古代深海沉积和遗迹化石群落.科学出版社,2003:1~231
晋慧娟,李育慈.深海沉积中的几种“特殊”原生沉积构造.中国科学(B辑),1998,25(8):890~896
晋慧娟,孙明良,李育慈.内蒙古桌子山中奥陶统的“特殊”浊积岩系.沉积学报,2005,23(1):34~40
李安仁,刘文均,张锦泉,等.鄂尔多斯盆地早奥陶世沉积特征及其演化.成都地质学院学报,1993,20(1):17~26
李斌,史晓颖,程长青,等.空间数据库技术在定量单因素作图法中的应用-以鄂尔多斯盆地奥陶系SQ17岩相古地理研究为例.煤田地质与勘探,2010,38(1):1~6
李春昱,王荃,张之孟,等.中国板块构造的轮廓.中国地质科学院院报,1980,2(1):11~20
李怀坤,耿建珍,郝爽,等.用激光烧蚀多接收器等离子体质谱仪(LA-MC-ICPMS)测定锆石U-Pb同位素年龄的研究.矿物岩石地球化学通报,2009b,28(增刊):77
李怀坤,陆松年,李惠民,等.侵入下马岭组的基性岩床的锆石和斜锆石U-Pb精确定年-对华北中元古界地层划分方案的制约.地质通报,2009a,28:1396~1404
李怀坤,苏文博,周红英,等.华北克拉通北部长城系底界年龄小于1670Ma-来自北京密云花岗斑岩岩脉锆石LA-MC-ICPMSU-Pb年龄的约束.地学前缘,2011,18:108~120
李怀坤,朱士兴,相振群,等.北京延庆高于庄组钾质斑脱岩的锆石U~Pb定年研究及其对华北北部中元古界划分新方案的进一步约束.岩石学报,2010,26:2131~2140
李建明,何幼斌,高振中,等.湖南桃江半边山前寒武纪内潮汐沉积及其共生沉积特征.石油天然气学报(江汉石油学院学报),2005b,27(5):545~547
李建明,王华,何幼斌,等.浙江临安上奥陶统复理石中的内潮汐沉积.石油天然气学报(江汉石油学院学报),2005a,27(1):1~4
李明瑞.鄂尔多斯盆地北部上古生界主要含气砂体沉积特征及储层控制因素研究.博士学位论文.成都:成都理工大学,2011.1~186
李少华,王彦宾,梁子斌,等.甘肃东南部地壳速度结构的区域地震波形反演.地球物理学报,2012,55(4):1186~1197
李文厚,陈强,李智超,等.鄂尔多斯地区早古生代岩相古地理.古地理学报,2012,14:85~100
李文厚,梅志超,陈景维,等.陕西渭北奥陶系放射虫硅质岩与火山钾质斑脱岩的成因环境.中国区域地质,1997,16:422~427
李祥辉,王成善,胡修棉.深海相中的砂质碎屑流沉积~以西藏特提斯喜马拉雅侏罗~白垩系为例.矿物岩石,2000,20(1):45~51
李向东,何幼斌,王丹,等.贺兰山以南中奥陶统香山群徐家圈组古水流分析.地质论评,2009a,55(5):653~662
李向东,何幼斌,王丹,等.宁夏中奥陶统香山群徐家圈组内波和内潮汐沉积.古地理学报,2009b,11(5):513~523
李向东,何幼斌,张铭记,等.宁夏中奥陶统香山群徐家圈组内波、内潮汐沉积类型.地球科学进展,2011,26(9):1006~1014
林畅松,杨起,李思田,等.贺兰奥拉槽早古生代深水重力流体系的沉积特征和充填样式.现代地质,1991,5(3):252~262
林畅松,杨起,李思田.贺兰拗拉槽盆地充填演化分析.北京:地质出版社,1995
刘宝宪,闫小雄,白海峰,等.鄂尔多斯盆地南缘中奥陶统平凉组成藏条件分析.天然气地球科学,2008,19:657~661
刘成鑫,高振中,纪友亮,等.鄂尔多斯盆地西南缘奥陶系深水牵引流沉积.海洋地质与第四纪地质,2005,25(2):31~36
刘德汉,付金华,郑聪斌,等.鄂尔多斯盆地奥陶系海相碳酸盐岩生烃性能与中部长庆气田气源成因研究.地质学报,2004,4:542~550
刘敦一,简平,张旗,等.内蒙古图林凯蛇绿岩中埃达克岩SHRIMP测年:早古生代洋壳消减的证据.地质学报,2003,77:317~327
刘浩军,薛典军,郭志宏,等.航空物探软件系统研制.物探与化探,2003,27(2):146~149
刘军锋,孙勇,孙卫东.秦岭拉鸡庙镁铁质岩体锆石LA~ICP~MS年代学研究.岩石学报,2009,25(2):320~330
刘钦甫,杨晓杰,丁述理.华北晚古生代煤系高岭岩微量元素和稀土元素地球化学研究.地球化学,1998,27(2):196~203
刘振军,张永军,赵百民.分带变倾角化极磁场图在大范围航磁解释中的应用.物探与化探,2010,34(2):221~224
马昌前,明厚利,杨坤光.大别山北麓的奥陶纪岩浆弧:侵入岩年代学和地球化学证据.岩石学报,2004,20:393~402
马杏垣,吴正文,谭应佳,等.华北地台基底构造.地质学报,1979,4:293~304
毛光周,刘池洋.地球化学在物源及沉积背景分析中的应用.地球科学与环境学报,2011,33(4):337~349
梅志超,陈景维,卢焕勇,等.陕西富平中奥陶统平凉组的深水碳酸盐碎屑流.石油与天然气地质,1982,3:49~56
孟祥化,葛铭.中朝板块层序·事件·演化.北京:科学出版社,2004:1~516
苗来成,刘敦一,张福勤,等.大兴安岭韩家园子和新林地区兴华渡口群和扎兰屯群锆石SHRIMPU-Pb年龄.科学通报,2007,52:591~601
宁夏回族自治区地质矿产局.宁夏回族自治区区域地质志.北京:地质出版社,1990:1~522
宁夏回族自治区地质矿产局.宁夏回族自治区岩石地层．武汉:中国地质大学出版社,1996:1~132
庞雄,陈长民,朱明,等.深水沉积研究前缘问题.地质论评,2007,53(1):36~43
裴福萍,许文良,杨德彬,等.松辽盆地基底变质岩中锆石U-Pb年代学及其地质意义.科学通报,2006,51:2882~2891
彭澎,翟明国.华北陆块前寒武纪两次重大地质事件的特征和性质.地球科学进展,2002,17:818~825
钱锋,艾永峰.鄂尔多斯南部地区早古生代主动大陆边缘演化特征.西安工程学院学报,2002,24:18~24
乔秀夫,张安棣.华北块体、胶辽朝块体与郯庐断裂.中国地质,2002,29(4):337~345
秦海鹏.北祁连造山带早古生代花岗岩岩石学特征及其与构造演化的关系.博士学位论文.北京:中国地质科学院,2012.1~141
屈红军,梅志超,李文厚,等.陕西富平地区中奥陶统等深流沉积的特征及其地质意义.地质通报,2010,29(9):1304~1309
阮小敏,孙若昧,滕吉文,等.鄂尔多斯及其周边地区地壳上地幔地震层析成像研究.中国地球物理学会第二十五届年会,2009,368
任纪舜等.中国东部及邻区大陆岩石圈的构造演化与成矿.北京:科学出版社,1990
ShanmugamG.深水砂体成因研究新进展.石油勘探与开发,2013c,40(3):294~301
陕西省地质矿产局.陕西省区域地质志.地质出版社,1989.1~698
陕西省地质矿产局.陕西省岩石地层.武汉:中国地质大学出版社,1998.1~291
施光海,刘敦一,张福勤,等.中国内蒙古锡林郭勒杂岩SHRIMP锆石U~Pb年代学及意义.科学通报,2003,48:2187~2192
史基安,邵毅,张顺存,等.鄂尔多斯盆地东部地区奥陶系马家沟组沉积环境与岩相古地理研究.天然气地球科学,2009,20(3):316~324
石玉若,刘敦一,张旗,等.内蒙古苏左旗地区闪长~花岗岩类SHRIMP年代学.地质学报,2004,78:789~799
宋凯,吕剑文,杜金良,等.鄂尔多斯盆地中部上三叠统延长组物源方向分析与三角洲沉积体系.古地理学报,2002,4(3):59~66
宋述光,张立飞,Y.Niu,等.北祁连山榴辉岩锆石SHRIMP定年及其构造意义.科学通报,2004,49:592~595
宋述光.北祁连山古大洋俯冲带高压变质岩研究评述.地质通报,2009,28:1769~1778
苏文博,李志明,EttensohnFR,JohnsonME,etal.华南五峰组-龙马溪组黑色岩系时空展布的主控因素及其启示.地球科学,2007,32(6):819~827
苏文博,李志明,史晓颖,等.华南五峰组-龙马溪组与华北下马岭组的钾质班脱岩及黑色岩系-两个地史转折期板块构造运动的沉积响应.地学前缘,2006,13(6):82~95
苏文博,何龙清,王永标,等.华南奥陶-志留系五峰组及龙马溪组底部斑脱岩与高分辨综合地层.中国科学D辑,2002(3):207~219
孙国凡,刘景平.贺兰坳拉槽与前渊盆地及其演化.石油与天然气地质,1983,4(3):236~245.
孙国凡,谢秋元，刘景平等.鄂尔多斯盆地的演化盈加与含油气性.石油与天然气地质,1986，7(4):356~366
孙晓猛,张旗,钱青.甘肃肃南白泉门地区蛇绿混杂岩地质特征.地球科学进展,1997,12(40):340~350
孙肇才,胡显穆.鄂尔多斯盆地西南缘奥陶系的对比划分意见及其对中西部油气勘探的意义.海相油气地质,2002,7:41~58
孙肇才,谢秋元.叠合盆地的发展特征及其含油气性—以鄂尔多斯盆地为例.石油实验地质,1980,1:3~21
滕吉文,王夫运,赵文智,等.鄂尔多斯盆地上地壳速度分布与沉积建造和结晶基底起伏的构造研究.地球物理学报,2008,51(6):1753~1766
王昌勇,郑荣才,王海红,等.鄂尔多斯盆地姬塬地区长6油层组物源区分析.沉积学报,2008,26(6):933~938
王官福,张文治.华北陆台北缘重磁异常的地质解释.物探与化探,1992,16:31~37
王国茹,陈洪德,朱志军,等.川东南~湘西地区志留系小河坝组砂岩稀土元素特征及其地质意义.石油实验地质,2010,32(5):487~495
王宏伟,何幼斌,孙宜显.甘肃夏河上二叠统内波、内潮汐沉积.石油天然气学报(江汉石油学院学报),2005,27(s4):561~562
王鸿祯.中国古地理图集.北京:地图出版社,1985:37~46
王鸿祯,何国琦,张世红.中国与蒙古之地质.地学前缘,2006,13(6):1~13
王鸿祯,刘本培,李思田.中国及邻区大地构造划分和构造发展阶段.见:王鸿祯,杨森楠,刘本培等著.中国及邻区构造古地理和生物古地理.武汉:中国地质大学出版社,1990:3~34
王鸿祯,莫宣学.中国地质构造述要.中国地质,1996:4~9
王鸿祯,杨森楠,李思田.中国东部及邻区中、新生代盆地发育及大陆边缘区的构造发展.地质学报,1983,3:213~223
王廷印,高军平,王金荣,等.内蒙古阿拉善北部地区碰撞期和后造山期岩浆作用.地质学报,1998,72(2):126~137
王涛,徐鸣洁,王良书,等.鄂尔多斯及邻区航磁异常特征及其大地构造意义.地球物理学报,2007,50:163~170
王志铄,王椿镛,曾融生,等.华北及邻区地壳上地幔三维速度结构的地震走时层析成像.CT理论与应用研究,2008,17(2):15~27
王少昌,付琐堂,李熙哲,等.鄂尔多斯盆地西缘古生代槽台过渡带裂谷系弧形构造带的形成与发展及对油气聚集富集规律的影响.天然气地球科学,2005,16(4):421~427
王同和.晋陕地区地质构造演化与油气聚集.华北地质矿产杂志,1995,10(3):283~398
王学平.鄂尔多斯南缘奥陶纪地层对比分析.陕西地质,2002,20:20~26
王玉新.鄂尔多斯地块早古生代构造格局及演化.地球科学:中国地质大学学报,1994,19(6):778~786
王振涛,周洪瑞,王训练,等.贺兰山地区中奥陶统樱桃沟组物源及构造背景分析.沉积学报,2014,32(2):205~217
魏魁生等著.碳酸盐岩层序地层学~以鄂尔多斯盆地为例.北京:地质出版社,2000,1~135
魏文博,金胜,叶高峰,等.华北地区大地电磁测深及岩石圈厚度讨论.中国地质,2006,33(4):762~772
吴胜和,冯增昭,张吉森.鄂尔多斯地区西缘及南缘中奥陶统平凉组重力流沉积.石油与天然气地质,1994,15(3):226~235
席胜利,郑聪斌,李振宏.鄂尔多斯盆地西缘奥陶系地球化学特征及其沉积环境意义.古地理学报,2004,6(2):196~206
夏林圻,夏祖春,徐学义.北祁连山奥陶纪弧后盆地火山岩浆成因.中国地质,2003,30(1):48~60
夏林圻,夏祖春,徐学义.北祁连山构造~火山~岩浆演化动力学.西北地质科学,1995,16:1~28
夏林圻,夏祖春,徐学义.北祁连山早古生代洋脊~洋岛和弧后盆地火山作用.地质学报,1998,72(4):301~312
夏明军,郑聪斌,毕建霞,等.鄂尔多斯盆地奥陶系生物礁及其天然气勘探前景.天然气地球科学,2008,19(2):178~182,271
辛勇光,周进高,邓红婴.鄂尔多斯盆地南部下奥陶统马家沟组沉积特征.海相油气地质,2010,15(4):1~5
许强,陈洪德,赵俊兴等.贺兰拗拉槽胡基台地区中奥陶统樱桃沟组深海重力流沉积特征.海相油气地质,2010,15(2):14~20
薛春纪,池国祥,薛伟,等.鄂尔多斯盆地生烃过程与流体流动及铀矿化关系.地学前缘,2011,18(5):19~28
许文彬,徐茂泉,孙美琴.等深流沉积研究现状与展望.台湾海峡,2004,23(3):394~402
许效松,徐强,潘桂棠,等.中国南大陆演化与全球古地理对比.北京:地质出版社,1996
许志琴,杨经绥,李海兵,姚建新.中央造山带早古生代地体构架与高压/超高压变质带的形成.地质学报,2006,80(12):1793~1805
闫全人,王宗起,闫臻,等.从华北陆块南缘大洋扩张到北秦岭造山带板块俯冲的转换时限.地质学报,2009,83:1565~1583
杨华,付金华,包洪平.鄂尔多斯地区西部和南部奥陶纪海槽边缘沉积特征与天然气成藏潜
力分析.海相油气地质,2010,15(2):1~13
杨江海,杜远生,朱杰.甘肃景泰崔家墩下奥陶统阴沟组砂岩化学组分特征及物源区构造背景判别.古地理学报,2007,9(2):197~206
杨江海.造山带碰撞~隆升过程的碎屑沉积响应:以北祁连志留系、右江二叠~三叠系和大别山南麓侏罗系为例.博士学位论文.武汉:中国地质大学(武汉),2012.1~151
杨俊杰,张伯荣.陕甘宁盆地油气区及油气藏序列.石油学报,1988,9(1):1~8
杨俊杰著.鄂尔多斯盆地构造演化与油气分布规律.北京:石油工业出版社,2002:1~85
杨森楠,姜本鸿,王祖春.华北与扬子陆块碰撞带构造古地理的特征和发展.见:王鸿祯,杨
森楠,刘本培等著.中国及邻区构造古地理和生物古地理.武汉:中国地质大学出版社,1990:165~186
杨遂正,金文化,李振宏.鄂尔多斯多旋回叠合盆地形成与演化.天然气地球科学,2006,17(4):494~498
杨婷,吴建平,房立华,等.华北地区地壳上地幔S波三维速度结构.地球物理学进展,2012,27(2):441~454
杨文敬.鄂尔多斯西缘奥陶纪沉积演化及其控制下的油气地质条件.硕士学位论文.西安:西北大学,2006.1~81
殷洪福,黄思骥,张克信,等.华南二叠纪~三叠纪之交的火山活动及其对生物灭绝的影响.地质学报,1989,63(2):169~180
袁鹤然,郑绵平,陈文西,张永生,等.陕北成盐盆地奥陶纪成钾找钾远景分析.地质学报,2010,84(11):1554~1564
袁卫国,赵一鸣.鄂尔多斯南部地区早古生代被动大陆边缘特征与演化.西北大学学报(自然科学版),1996,26:451~454
袁卫国．鄂尔多斯盆地南缘中奥陶统火山钾质斑脱岩的研究与意义.石油实验地质,1995,17:167~170
袁效奇,耿国仓.巴彦浩特盆地东部古生代沉积的发现及其大地构造意义.石油与天然气地质,1992,13(4):381~389
袁照令,李大明.关于磁异常化到地磁极问题的几点认识.物探化探计算技术,1998,20(3):284
翟明国.华北克拉通的形成演化与成矿作用.矿床地质,2010,29:24~36
翟明国.华北克拉通中生代破坏前的岩石圈地幔与下地壳.岩石学报,2008,24(10):2185~2204
张福礼.鄂尔多斯盆地早古生代复合的古构造体系与天然气.地质力学学报,2002,8(3):193~2000张泓,白清昭,张笑微,等.鄂尔多斯聚煤盆地形成与演化.西安:陕西科学技术出版社,1995
张进,李锦轶,刘建峰,等.早古生代阿拉善地块与华北地块之间的关系:来自阿拉善东缘中奥陶统碎屑锆石的信息.岩石学报,2012,28(9):2912~2934
张进,马宗晋,任文军.再论贺兰山地区新生代之前拉张活动的性质.石油学报,2004,25:8~11张抗.鄂尔多斯断块构造和资源.西安:陕西科学技术出版社,1989:7~8,29~81,193~250
张抗.鄂尔多斯断块太古代至早元古代构造发育特征.地质科学,1982:352~363
张抗.鄂尔多斯盆地西、南缘奥陶系滑塌堆积.沉积学报,1992,10(1):11~18
张抗.论贺兰裂堑.见:鄂尔多斯盆地西缘地区石油地质论文集.呼和浩特:内蒙古人民出版社,1983:29~40
张旗,孙晓猛,周德进,等.北祁连蛇绿岩特征、形成环境及其构造意义.地球科学进展,1997a,12(4):366~393
张旗,王岳明,钱青,等.甘肃景泰县老虎山地区蛇绿岩及其上覆岩系中枕状熔岩的地球化学特征.岩石学报,1997,13:92~99
张道峰,杨文敬,漆亚玲,等.鄂尔多斯盆地神木地区上古生界山西组物源分析.天然气地球科学,2009,20(6):902~906
章贵松,张军,任军峰,等.六盘山弧形冲断体系构造新认识.新疆石油地质,2006,27(5):542~544
张国伟,张本仁,袁学诚,等.秦岭造山带与大陆动力学.北京:科学出版社,2001
张吉森,费安琦,王志辉.鄂尔多斯西、南部中奥陶世环陆架沉积特征.石油与天然气地质,1982,3(4):360~368
张家声,李燕,黄雄南.中国北部古元古代地壳尺度的伸展拆离和硅铝壳内活动带:北东向线性航磁异常的地质构造解释.地质科学,2007,42:267~302
张家声,索书田.华北北部结晶基底中的大型韧性剪切带.中国区域地质,1988(4),289~296
张建新,许志琴,陈文,等.北祁连中段俯冲~增生杂岩/火山弧的时代探讨.岩石矿物杂志,1997,16:112~119
张金川.鄂尔多斯盆地构造演化及含油气展望.天然气地质,1982,3(4):304~315
张俊明,李国祥,周传明.滇东下寒武统含磷岩系底部火山喷发事件沉积及其意义.地层学杂志,1997,21(2):91~99,155
张俊明,李国祥,周传明.滇东早寒武世梅树村期浅角粘土岩层的地球化学特征和地质意义.岩石学报,1997,13(1):100~110
张培琴,赵群友.低磁纬度区航磁异常变倾角磁方向转换方法.物探化探计算技术,1996,18(3):206
张勤文,徐道一.地层界线上灾变事件标志和成因的探讨.地球学报,1994,15(3/4):192~199
张锡林,姚长利.低磁纬度地区磁异常化极方法及应用.石油物探,2003,42(4):541
张先,李长法,贺为民.鄂尔多斯北缘地震带地壳磁性层特征.见:中国地球物理学会第七届学术年会论文集,1991
张永军,张开均.根据航磁数据探讨阿尔金断裂带的结构及构造演化.物探与化探,2007,31(6):489~494
赵国春.华北克拉通基底主要构造单元变质作用及其若干问题讨论.岩石学报,2009,25(8):1172~1792
赵国泽,詹艳,王立凤,等.鄂尔多斯断块地壳电性结构.地震地质,2010,32(3)345~359
赵红格,刘池洋,王峰,等.鄂尔多斯盆地西缘构造分区及其特征.石油与天然气地质,2006,27(2):173~179
赵振宇,郭彦如,王艳,等.鄂尔多斯盆地构造演化及古地理特征研究进展.特种油气田,2012,19(5):15~20
赵重远.鄂尔多斯地块西缘构造演化及板块应力机制分析.见:鄂尔多斯盆地西缘地区石油地质论文集.呼和浩特:内蒙人民出版社,1983:20~28
赵宗溥,等.中朝准地台前寒武纪地壳演化.北京:科学出版社,1993.366~388
郑绵平,齐文,张永生.中国钾盐地质资源现状与找钾方向初步分析.地质通报,2006a,5(11):1239~1246
郑绵平,袁鹤然,赵希涛,等.青藏高原第四纪泛湖期与古气候.地质学报,2006b,80(2):169~180
郑绵平,袁鹤然,张永生,等.中国钾盐区域分布与找钾远景.地质学报,2010,84(11):1523~1553
郑昭昌,李玉珍.贺兰山奥陶系研究的新进展.现代地质,1991,6(5):119~137
《中国石油天然气的勘查与发现》编辑部.中国石油天然气的勘查与发现.北京:地质出版社,1992
周安朝.华北地块北缘晚古生代盆地演化及盆山耦合关系.博士学位论文.西安:西北大学,2000.1~144
周立宏,李三忠,刘建忠,等.渤海湾盆地区燕山期构造特征与原型盆地.地球物理学进展,2003,18(4):692~699
周书昌,冯乔,赵伟,等.鄂尔多斯盆地南缘岐山剖面中奥陶统平凉组沉积环境分析.沉积与特提斯地质,2011,31:28~33
周进高,张帆,郭庆新,等.鄂尔多斯盆地下奥陶统马家沟组障壁潟湖沉积相模式及有利储层分布规律.沉积学报,2011,29(1):64~71
周民都,王椿镛,曾融生.青藏高原东北缘地壳上地幔速度结构的地震层析成像研究.西北地震学报,2012,34(3):224~233
周喜文,赵国春,耿元生.贺兰山高压泥质麻粒岩-华北克拉通西部陆块拼合的岩石学证据.岩石学报,2010,26(7),2113~2121
朱光,胡召齐,陈印,等.华北克拉通东部早白垩世伸展盆地的发育过程及其对克拉通破坏的指示.地质通报,2008,27(17):1594~1604
朱如凯,孟祥化,葛铭.巴彦浩特盆地东缘中奥陶统混合型深水重力流沉积层序及其旋回.沉积学报,1994,12(2):77~85
左朝国,刘义科,张崇.北祁连造山带中-西段陆壳残块群的构造-地层特征.地质科学,2002,37:302~312
Anderson T. Correction of common lead in U-Pb analyses that do not report204Pb. Chemical Geology,2002,192:59-79
Badenas B, Pomar L, Aurell M et al. A facies model for internalites (internal wave deposits) on a gently sloping carbonate ramp (Upper Jurassic, Ricla, NE Spain). Sedimentary Geology,2012,271-272:44-57
Bahadur R A M, Singh N P, Murthy A S K. Aeromagnetic Anomalies Uncover the Precambrian Basement in the Chhattisgarh Basin Area, Central India. Acta Geophysica,2008,56:982-993
Bergstrom S M, Huff W D, Kolata D R. The Lower Silurian Osmundsberg K-bentonite. Part I: stratigraphic position, distribution, and palaeogeographic significance. Geological Magazine,1997,135:1-13
Bhatia M R, Crook K A. Trace Element Characteristics of Graywackes and Tectonic Setting Discrimination of Sedimentary Basins. Contributions to Mineralogy and Petrology,1986,90(2):181-193
Bhatia M R, Taylor S R. Trace-element Geochemistry and Sedimentary Provinces:a Study from the Tasman Geosyncline, Australia. Chemical Geology,1981,33(1/2):115-125
Bhatia M R. Plate Tectonics and Geochemical Composition of Sandstones. The Journal of Geology,1983,91(6):611-627
Bhatia M R. Rare Earth Element Geochemistry of Australian Paleozoic Graywackes and Mudrocks:Provenance and Tectonic Control. Sedimentary Geology,1985,45(1/2):97-113.
Boynton W V. Cosmochemistry of the rare earth elements:Meteorite studies. Dev Geochem,1984,2:63-114
Calarge L M, Meunier A, Formoso ML L. A bentonite bed in the Acegua (RS, Brazil) and Melo (Uruguay) areas:a highly crystallized montmorillonite. Journal of South American Earth Scienees,2003,16:187-198
Carlson R W, Pearson D G, James D E. Physical, Chemical, and chronological characteristics of continental mantle. Reviews of Geophysics,2005,43, RG1001, doi:10,1029/2004RG000156
Carroll A R, Grahamwand S A, Smith M E. Walledsedimentary basinsof China, BasinResearch,2010,22:17-32
Chen L. Lithospheric structure variations between the eastern and central North China Craton from S-and P-receiver function migration. Physics of the Earth and Planetary Interiors2009,173:216-227
Chen L, Cheng C, Wei Z G. Seismic evidence for significant lateral variations in lithospheric thickness beneath the central and western North China Craton. Earth and Planetary Science Letters,2009a,286:171-183
Chen L, Sun Y, Diwu C R, Wang H L. Crust for mation in the Ordos block:Constraints from detrital zircons from Ordovican and Permian sandstones. In:Abstract with Program of International Discussion meeting on Continental Geology and Tectonics. Northwest University Press, Xi'an,2009b.17
Chen L, Wang T, Zhao L, et al. Distinct lateral variation of lithospheric thickness in the Northeastern North China Craton. Earth and Planetary Science Letters2008,267:56-68
Chen L, Zheng T Y, Xu W W. A thinned lithospheric image of the Tanlu Fault Zone, eastern China: Constructed from wave equation based receiver function migration. Journal of Geophysical Research2006,111:B09312,doi:10.1029/2005JB003974
Cheng C, Chen L, Yao H J, et al. Distinct variations of crustal shear wave velocity structure and radial anisotropy beneath the North China Craton and tectonic implications. Gondwana Research,2013,23:25-38
Compston W. Interpretations of SHRIMP and isotope dilution zircon ages for the geological time-scale:1. The early Ordovician and late Cambrian. Mineralogical Magazine,2000,64(1):43-57
Condie K C. Another look at rare earth elements in shales. Geochimica et Cosmochimica Acta,1991,55:2527-2531
Darby B J, Gehrels G E. Detrital zircon reference for the North China block. Journal of Asian Earth Sciences,2006,26:637-648
Darby B J, Ritts B D. Mesozoic contractional deformation in the middle of the asian tectonic collage; the intraplate western Ordos Fold-Thrust Belt, China. Earth and Planetary Science Letters2002,205:13-24
Desmares D, Grosheny D, Beaudoin B, et al. High resolution stratigraphic record constrained by volcanic ash beds at the Cenomanian-Turonian boundary in the Western Interior basin, USA. Cretaceous Research,2007,28:561-582
Dickinson W R, Gehrels G E. U-Pb ages of detrital zircons in Jurassic eolian and associated sandstones of the Colorado Plateau:Evidence for transcontinental dispersal and intraregional recycling of sediment. Geological Society of America Bulletin,2009,121:408-433
Dickinson W R, Suczek C A. Plate tectonics and sandstone compositions. The American Association of Petroleum Geologists Bulletin,1997,63(12):2164-2182
Dickinson W R. Interpreting provenance relations from detrital modes of sandstones. In:Zuffa G G ed. Provenance of Arenites. Dordrecht:D. Reidel, NA TO-ASI Series1985,148:333-361
Dickinson W R. Provenance of North American Phanerozoic sandstones in relation to tectonic setting. GSA Bulletin,1983,94:222-235
Diwu C R, Sun Y, Zhang H, et al. Episodic tectonothermal events of the western North China Craton and North Qinling Orogenic Belt in central China:Constraints from detrital zircon U-Pb ages. Journal of Asian Earth Sciences2012,47:107-122
Dohan K, Sutherland B R. Numerical and laboratory generation of internal waves from turbulence. Dynamics of Atmospheres and Oceans,2005,40:43-56
Dong H L, Hall C M, Halliday A N, et al.40Ar/39Ar illite dating of Late Caledonian(Acadian) metamorphism and cooling of K-bentonites and slate from the Welsh basin, UK. Earth and Planetary Science Letters,1997,150:337-351
Du Y, Wang J, Han X, et al. From flysch to molasse-the sedimentary and tectonic evolution of the late Caledonian-early Hercynian foreland basin in North Qilian Mountains. Journal of China University of Geosciences,2003,13(1):1-7
Du L L, Yang C H, Wang W, et al. Paleoproterozoic rifting of the North China Craton: Geochemical and zircon Hf isotopic evidence from the2137Ma Huangjinshan A-type granite porphyry in the Wutai area. Journal of Asian Earth Sciences2013,72:190-202
Enkelmann E, Weislogel A, Ratschbacher L, et al. How was the Triassic Songpan-Ganzi Basin filled? A provenance study. Tectonics,2007,26, TC4007:1-24
Fang L F, Wu J P, Ding Z F, et al. Crustal velocity structures beneath North China revealed by ambient noise tomography. Earthquake Science2010,23:477-486
Faure M, Lin W, Monie P, Bruguier O. Palaeoproterozoic arc magmatism and collision in Liaodong Peninsula (northeast China). Terra Nova2004,16:75-80
Faure M, Trap P, Lin W, Monie P, Bruguier O. Polyorogenic evolution of the Paleoproterozoic Trans-North China Belt, new insights from the Luliangshan-Hengshan-Wutaishan and Fuping massifs. Episodes2007,30:1-12
Fleet A R. Aqueous and sedimentary geochemistry of the rare earth elements. In:Henderson P.(ed.),Rare Earth Element Geochemistry, Elsevier,1984:331-373
Foreman B Z, Rogers R R, Deino A L, et al. Geochemical characterization of bentonite beds in the two Medicine Formation (Campanian, Montana), in eluding a new40Ar/39Ar age. Cretaceous Research,2007, doi:10.1016/j.cretres2007.07.001
Gao Z Z, Eriksson K A, He Youbin, et al. Deep-Water Traction Current Deposits-A Study of Internal Tides, Internal Waves, Contour Currents and Their Deposits. Beijing and New York: Science Press, Utrecht and Tokyo:VSP,1998
Gao Z Z, Eriksson K A. Internal-tide deposits in an Ordovician submarine channel:Previously unrecognized facies?. Geology,1991,19(7):734-737
Gao Z Z, He Y B, Li J M, et al. The first internal-tide deposits found in China. Chinese Science Bulletin,1997,42(13):1113-1117
Gehrels G E, Yin A, Wang X F. Detrital zircon geochronology of the northeastern Tibetan Plateau. Geological Society of America Bulletin,2003,115:881-896
Gerkema T, Lam F P A, Maas L R M. Internal tides in the Bay of Biscay:conversion rates and seasonal effects. Deep-Sea Research Ⅱ,2004,51(25/26):2995-3008
Gerkema T, Staquet C, Bouruet Aubertot P. Nonlinear effects in internal-tide beams, and mixing. Ocean Modelling,2006,12:302-318
Girty G H, Hanson A D, Knaack C, et al. Provenance Determined by REE, Th, and Sc Analyses of Metasedimentary Rocks, Boyden Cave Roof Pendant, Central Sierra Nevada, California. Journal of Sedimentary Research,1994,64(1):68-73
Gradstein F M, Ogg J G and Smith A G. A Geologic Time Scale. Camdridge:Cambridge University Press,2004.1-589
Guo J H, Peng P, Chen Y, et al. UHT sapphirine granulite metamorphism at1.93-1.92Ga caused by gabbronorite intrusions:implications for tectonic evolution of the northern margin of the North China Craton. Precambrian Research,2012, doi.org/10.1016/j. precamres.2011.07.020
Guo J H, Sun M, Chen F K, et al. Sm\Nd and SHRIMP U\Pb zircon geochronology of high-pressure granulites in the Sanggan area, North China Craton:timing of Paleoproterozoic continental collision. Journal of Asian Earth Sciences,2005,24:629-642
Haughton P D, Todd S P, Morton AC. Sedimentary provenance studies. Geological Society, London, Special Publications.1991,57:1-11
Haynes J T, Melson W G, Kunk M J. Composition of biotite phenocrysts in Ordovician tephras casts doubt on the proposed trans. Atlantic correlation of the Millbrig K-bentonite (United States) and the Kinnekulle K-bentonite (Sweden). Geology,1995,23(9):847-850
He Y B, Luo J X, Gao Z Z, et al. Reply to the Discussion of He et al.(2011, Geo-Marine Letters) Evidence of internal-wave and internal-tide deposits in the Middle Ordovician Xujiajuan Formation of the Xiangshan Group, Ningxia, China. Geo-Marine Letters,2012,32:367-372
He Y B, Luo J X, Li X D, et al. Evidence of internal-wave and internal-tide deposits in the Middle Ordovician Xujiajuan Formation of the Xiangshan Group, Ningxia, China. Geo-Marine Letters,2011,31:509-523
He Y B, Gao Z Z. The Characteristics and recognition of internal-tide and internal-wave deposits. Chinese Science Bulletin,1999,44(7):582-589
Helge J H, Harald F, Ole J M. Paleogene tuffaceous intervals, Grane Field(Block25-11), Norwegian North Sea:their depositional, petrographical, geochemical character and regional implications. Marine and Petroleum Geology,2000,17:101-118
Hendrix M S. Evolution of Mesozoic sandstone compositions, Southern Junggar, Northern Tarim, and Western Turpan Basins, Northwest China:A detrital record of the ancestral Tian Shan. Journal of Sedimentary Research,2000,70(3):520-532
Hu Y H, Zhou J B, Song B, et al. SHRIMP zircon U-Pb dating from K-bentonite in the top of Ordovician of Wangjiawan Section, Yichang, Hubei, Science China (D),2008,51(4):493-498
Hu J M, Liu X S, Li Z H, et al.. SHRIMP U-Pb zircon dating of the Ordos Basin basement and its tectonic significance. Chinese Science Bulletin2012,57, doi:10.1007/s11434-012-5274-0
Huang X L, Zhong J W, Xu Y G. Two tales of the continental lithospheric mantle prior to the destruction of the North China Craton:Insights from Early Cretaceous mafic intrusions in western Shandong, East China. Geochimica et Cosmochimica Acta,2012,96:193-214
Huertas M O, Palomo I,Moresi M,et al. A mineralogical and geochemical approach to establish a sedimentary model in a passive continental margin Sabbetic Zone, Betic Cordilleras, Sepein. Clay Minerals,1991,26:389-407
Huff W D, Bergstrom S M, Kolata D R, et al. The Lower Silurian Osmundsberg K-bentonite. Part Ⅱ:mineralogy, geochemistry, chemo stratigraphy and tectonomagmatic significance. Geological Magazine,1997b,135:15-26
Huff W D, Bergstrom S M, Kolata D R. Gigantic Ordovician volcanic ash fall in North Amerrica and Europe:Biological, tectonomagmatic, and event-stratigraphic significance. Geology,1992,20:875-878
Huff W D, Bergstrom S M, Kolata D R. Silurian K-bentonites of the Dnestr Basin, Podolia, Ukraine. Journal of the Geological Society,2000,157:493-504
Huff W D. Ordovician K-bentonites:Issues in interpreting and correlating ancient tephras. Quaternary International,2008,178:276-287
Huff W D, Bergstrm S M, Kolata D R. Gigantic Ordovician volcanic ash fall in North America and Europe:Biological, tectonomagmatic, and event-stratigraphic significance. Geology,1992,20(10):875-878
Jackson S E, Pearson N J, Griffin W L, et al. The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U-Pb zircon geochronology. Chemical Geology,2004,211:47-69
Jia C Z, Li B L, Zhang X Y, et al. Formation and evolution of the Chinese marine basins. Chinese Science Bulletin,2007,52:1-11
Jian P, Liu D Y, Kroner A, et al. Time scale of an Early to Mid-Paleozoic orogenic cycle of the long-lived Central Asian Orogenic Belt, Inner Mongolia of China:implications for continental growth. Lithos,2008,101:233-259
Johnson A C, Swain C J. Further evidence of fracture-zone induced tectonic segmentation of the Antarctic Peninsula from detailed aeromagnetic anomalies. Geophysical Research Letters1995,22:1917-1920
Kolata D R, Huff W D, Bergstrom S M. Nature and regional significance of unconformities associated with the Middle Ordovician Hagan K-bentonite complex in the North American midcontinent. Geological Society of America Bulletin,1998,110:723-739
Kroner A, Wilde S A, Li J H, et al. Age and evolution of a late Archaean to early Palaeozoic upper to lower crustal section in the Wutaishan/Hengshan/Fuping terrain of northern China. Journal of Asian Earth Sciences2005a,24:577-595
Kroner A, Wilde S A, O'Brien P J, et al. Feild relationships, geochemistry, zircon ages and evolution of a late Archean to Paleoproterozoic lower crustal section in the Hengshan Terrain of Northern China. Acta Geologica Sinica (English Edition)2005b,79:605-629
Kroner A, Wilde S A, Zhao G C, et al. Zircon geochronology of mafic dykes in the Hengshan Complex of northern China:evidence for late Palaeoproterozoic rifting and subsequent high-pressure event in the North China Craton. Precambrian Research2006,146:45-67
Kusky T M. Geophysical and geological tests of tectonic models of the North China Craton. Gondwana Research2011a,20:26-35
Kusky T M. Comparison of results of recent seismic profiles with tectonic models of the North China craton. Journal of Earth Sciences2011b,22:250-259
Kusky T M, Li J H. Paleoproterozoic tectonic evolution of the North China Craton. Journal of Asian Earth Sciences2003,22:383-397
Kusky T M., Li J H, Santosh M. The Paleoproterozoic North Hebei Orogen:North China Craton's collisional suturewith the Columbia supercontinent. Gondwana Research2007,12:4-28
Kusky T M, Santosh M. The Columbia connection in North China. In:Reddy, S.M., Mazumder, R., Evans, D., Collins, A.S.(Eds.), Paleoproterozoic Supercontinents and Global Evolution Geological Society of London, Special Publication,2009,323:49-71
Kusky T M, Li J H, Tucker R D. The Archean Dongwanziophiolitecomplex, North ChinaCraton:2.505billion year old oceanic crust andmantle. Science2001,292:1142-1145
Lan T G, Fan H R, Hu F F, et al. Multiple crust-mantle interactions for the destruction of the North China Craton:Geochemical and Sr-Nd-Pb-Hf isotopic evidence from the Longbaoshan alkaline complex. Lithos2011,122:87-106
Li S G, Huang F, Nie Y H, et al. Geochemical and geochronological constraints on the suture location between the North and South China blocks in the Dabie orogen, central China. Physics and Chemistry of the Earth,2001,26:655-672
Li H K, Lu S N, Su W B, et al. Recent advances in the study of the Mesoproterozoic geochronology in the North China Craton. Journal of Asian Earth Sciences2013a,72:216-227
Li H Y. Destruction of North China Craton:Insights from temporal and spatial evolution of the proto-basins and magmatism. Science China Earth Sciences,2013,56(3):464-478
Li H Y, Xu Y G, Liu Y M, et al. Detrital zircons reveal no Jurassic plateau in the eastern North China Craton. Gondwana Research2013b,24:622-634
Li J W, Bi S J, Selby D, et al. Giant Mesozoic gold provinces related to the destruction of the North China craton. Earth and Planetary Science Letters,2012a,349-350:26-37
Li M, Gao J R. Basement faults and volcanic rock distributions in the Ordos Basin. Science China: Earth Sciences,2010, doi:10.1007/s11430-010-4042-8
Li S Z, Zhao G C, Dai L N, et al. Cenozoic faulting of the Bohai Bay Basin and its bearing on the destruction of the eastern North China Craton. Journal of Asian Earth Sciences,2012b,47:80-93
Li X P, Yang Z Y, Zhao G C, et al. Geochronology of khondalite-series rocks of the Jining Complex:confirmation of depositional age and tectonometamorphic evolution of the North China craton. International Geology Review,2011,53:1194-1211
Li, Z W, Hao T Y, Xu Y. Uppermost mantle structure of the North China Craton:Constraints from interstation Pn travel time difference tomography. Chinese Science Bulletin2011,56, doi:10.1007/s11434011-4487-y
Lin W, Wang Q C, Wang J, et al. Late Mesozoic extensional tectonics of the Liaodong Peninsula massif:Response of crust to continental lithosphere destruction of the North China Craton. SCIENCE CHINA Earth Sciences,2011,54:843-857
Ling M X, Li Y, Ding X, et al. Destruction of the North China Craton Induced by Ridge Subductions. Journal of Geology,2013,121(2):197-213
Liu Y S, Gao S, Hu Z C, et al. Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen:U-Pb dating, Hf isotopes and trace elements in zircons from mantle xenoliths. Journal of Petrology,2009,51:537-571
Lv B, Zhai M G, Li T S, et al. Zircon U\Pb ages and geochemistry of the Qinglong volcano～sedimentary rock series in Eastern Hebei:implication for～2500Ma intra～continental rifting in the North China Craton. Precambrian Research,2012,208-211:145-160
Lu Y F, Xu M J, Wang L S, et al. Crustal structure of the southeastern margin of the OrdosBlock. Chinese Science Bulletin2011,56:3854-3859, doi:10.1007/s11434-011-4847-7
Ludwig K R. User's manual for Isoplot/Ex, version3.00. A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronology Center Special Publication,2003,4:1-70
Mao J W, Zhang Z C, Zhang Z H, et al. Re-Os isotopic dating of molybdenites in Xiaoliugou W(Mo) deposit in the northern Qilian mountains and its geological significance. Geochemical et Cosmochemica Acta,1999,63:1815-1818
Mao J W, Zhang Z H, Jian P, et al. U-Pb zircon dating of the Yeniutan granitic intrusion in the western sector of the North Qilian Mountains. Acta Geologica Sinica,2000,74:781-785
Marker P G, Huff W D. What is a K-bentonite? Geological Society of America Abstracts with Programs,2005,37:143
McLennan S M. Rare earth elements in sedimentary rocks:influence of provenance and sedimentary processes. In:Lipin B R and McKay G A (eds). Geochemistry and mineralogy of rare earth elements. Mineralogical Society of America,1989,21:169-200
Najman Y. The detrital record of orogenesis:A review of approachs and techniques used in the Himalayan sedimentary basins. Earth-Science Reviews,2006,74:1-72
Pearce J A, Harris N B W, Tindle A G. Trace element discrimination diagrams for the tectonic
interpretation of granitic rocks. Journal of Petrology,1984,25:956-983
Pearce J A, Norry M J. Petrogenetic implications of Ti, Zr, Y, and Nb variations in volcanic rocks. Contributions to Mineralogy and Petrology,1979,69:33-47
Pei F P, Xu W L, Yang D B, et al. Geochronology and geochemistry of Mesozoic mafic-ultramafic complexes in the southern Liaoning and southern Jilin provinces, NE China:Constraints on the spatial extent of destruction of the North China Craton. Journal of Asian Earth Sciences, 2011,40:636-650
Peng P, Guo J H, Windley B F, et al. Halaqin volcano-sedimentary succession in the central-northern margin of the North China Craton:products of Late Paleoproterozoic ridge subduction. Precambrian Research,2011,187:165-180
Peng T P, Fan W M, Peng P X. Geochronology and geochemistry of late Archean adakitic plutons from the Taishan granite-greenstone Terrain:implications for tec-tonic evolution of the eastern North China Craton. Precambrian Research,2012,208-211:53-71
Pomar L, Morsilli M, Hallock P, et al. Internal waves, an under-explored source of turbulence events in the sedimentary record. Earth-Science Reviews,2012,111:56-81
Pomar L, Morsilli M, Hallock P, et al. Reply to Shanmugam, G., comment on "Internal waves, an underexplored source of turbulence events in the sedimentary record" by Pomar et al.[Earth-Science Reviews,111(2012),56-81], Earth Science Reviews (2012). Earth-Science Reviews,2013,116:206-210
Ram B, Singh N P, Murthy A S K. A note on the qualitative appraisal of aeromagnetic image of Chhattisgarh basin. Journal of Indian Geophysical Union,2007,11:129-133
Ray R D, Mitchum G T. Surface manifestation of internal tides in the deep ocean:observations from altimetry and island gauges. Progression of Oceanography,1997,40:135-162
Ren L D, Geng Y S, Du L L, et al. SHRIMP data on zircons from the Wanzi series:Constraints on the rock formation time and implications of migmatization at2.1-2.0Ga in the Fuping Complex, North China Craton. Journal of Asian Earth Sciences,2013,72:203-215
Ribbe J, Holloway P E. A model of suspended sediment transport by internal tides. Continental Shelf Research,2001,21:395-422
Roser B P, Korsch R J. Determination of Tectonic Setting of Sandstone-mudstone Suites Using SiO2Content and K20/Na2O Ratio. The Journal of Geology,1986,94(5):635-650
Santosh M. Assembling North China Craton within the Columbia superconti～nent:the role of double-sided subduction. Precambrian Research,2010,178:149-167
Santosh M, Kusky T M. Origin of paired high pressure-ultrahigh-temperature orogens:a ridge subduction and slab window model. Terra Nova,2010,22:35-42
Santosh M, Liu S J, Tsunogae T, et al. Paleoproterozoic ultrahigh-temperature granulites in the North China Craton:implications for tectonic models on extreme crustal metamorphism. Precambrian Research,2012. http://dx.doi.org/10.1016/j.precamres.2011.05.003
Santosh M, Sajeev K, Li J H. Extreme crustal metamorphism during Columbia supercontinent assembly:evidence from North China Craton. Gondwana Research2006,10:256-266
Santosh M, Sajeev K, Li J H, et al. Counterclockwise exhumation of a hot orogen:the Paleoproterozoic ultrahigh-temperature granulites in the North China Craton. Lithos,2009a,110:140-152
Santosh M, Tsunogae T, Li J H. Discovery of sapphirine-bearing Mg-Al granulites in the North China Craton:implications for Paleoproterozoic ultrahigh temperature metamorphism. Gondwana Research,2007a,11:263-285
Santosh M, Tsunogae T, Ohyama H, et al. Carbonic meta-morphism at ultrahigh-temperatures: evidence from North China Craton. Earth and Planetary Science Letters,2008,266:149-165.
Santosh M, Wan Y, Liu D, et al. Anatomy of zircons from an ultrahot Orogen:the amalgamation of North China Craton within the supercontinent Columbia. Journal of Geology,2009a,117:429-443
Santosh M, Wilde S A, Li J H. Timing of Paleoproterozoic ultrahigh temperature metamorphism in the North China Craton:evidence from SHRIMP U-Pb zircon geochronology. Precambrian Research,2007b,159:178-196
Santosh M, Zhao D P, Kusky T M. Mantle dynamics of the Paleoproterozoic North China Craton: a perspective based on seismic tomography. Journal of Geodynamics2010,49:39-53
Shanmugam G. Discussion of He et al.(2011, Geo-Marine Letters) Evidence of internal-wave and internal-tide deposits in the Middle Ordovician Xujiajuan Formation of the Xiangshan Group, Ningxia, China. Geo-Marine Letters,2012,32:359-366
Shanmugam G. Modern internal waves and internal tides along oceanic pycnoclines:Challenges and implications for ancient deep-marine baroclinic sands. AAPG Bulletin,2013b,97(5):799-843
Shanmugam G. New perspectives on deep-water sandstones:Implications. Petroleum Exploration and Development,2013a,40(3):316-324
Shen J F, Santosh M, Li S R, et al. The Beiminghe skarn iron deposit, eastern China: Geochronology, isotope geochemistry and implications for the destruction of the North China Craton. Lithos,2013,156-159:218-229
Shi Y, Yu J H, Santosh M. Tectonic evolution of the Qinling orogenic belt, Central China:New evidence from geochemical, zircon U-Pb geochronology and Hf isotopes. Precambrian Research,2013,231:19-60
Song S G, Niu Y, Zhang L F, et al. Tectonic evolution of early Paleozoic HP metamorphic rocks in the North Qilian Mountains, NW China:new perspectives. Journal of Asian Earth Sciences.2009,35:334-353
Song S G, Niu Y L, Su L, et al. Tectonics of the North Qilian orogen, NW China. Gondwana Research,2013,23:1378-1401
Su W B, He L Q, Wang Y B, et al. K-bentonite beds and high-resolution integrated stratigraphy of the uppermost Ordovician Wufeng and the lowest Silurian Longmaxi formations in South China. SCIENCE CHINA:Earth Sciences,2003,46:1121-1133
Su W B, Huff W D, Frank R E, et al. K-bentonite, black shale and flysch successions at the Ordovician-Silurian transition, South China:Possible sedimentary responses to the accretion of Cathaysia to the Yangtze Block and its implications for the evolution of Gondwana. Gondwana Research,2009, doi:10.1016/j.gr.2008.06.004
Su W B, Li H K, Huff W D, et al. SHRIMP U-Pb dating for a K-bentonite bed in the Tieling Formation, North China. Chinese Science Bulletin,2010,55:3312-3323
Su W B, Zhang S H, Huff W D, et al. SHRMP U-Pb ages K-bentuonite beds in the Xiamaling Formation:Implications for revised subdivision of the Meso-to Neoproterozoic history of the North China Craton. Gondwana Research,2008, doi:10.101b/j.gr.2008.04.007
Sun W D, Li S G, Sun Y, et al. Mid-paleozoic collision in the north Qinling:Sm-Nd, Rb-Sr and40Ar/39Ar ages and their tectonic implications. Jounal of Asian Earth Sciences,2002,21:69-76
Sun Z, Xie Q, and Yang J. Ordos basin-A typical example of an unstable cratonic interior superimposed basin, in X. Zhu and W. Xu, eds., Chinese sedimentary basins:Amsterdam, Elsevier,1989.148-168
Sutherland B R, Hughes G O, Dalziel S B, et al. Internal waves revisited. Dynamics of Atmospheres and Oceans,2000,31:209-232
Taylor S R, Mclennan S M. The continental crust:its composition and evolution:An examination of the geochemical record preserved in sedimentary rocks. Oxford:Blackwell Scientific Publications,1985
Tian Y, Zhao D P. Destruction mechanism of the North China Craton:Insight from P and S wave mantle tomography. Journal of Asian Earth Sciences,2011,42:1132-1145
Tian Y, Zhao D P, Sun R M, et al. Seismic imaging of the crust and upper mantle beneath the North China Craton. Physics of the Earth and Planetary Interiors,2009,172:169-182
Tseng C Y, Yang H J, Yang H Y, et al. Continuity of the North Qilian and North Qinling orogenic belts, Central Orogenic System of China:Evidence from newly discovered Paleozoic adakitic rocks. Gondwana Research,2009,16:285-293
Wan Y S, Dong C Y, Liu D Y, et al. Zircon ages and geochemistry of late Neoarchean syenogranites in the North China Craton:A review. Precambrian Research,2012. http://dx.doi.org/10.1016/j.precamres.2011.05.001
Wan Y S, Liu D Y, Wang S J, et al.2.7Ga juvenile crust formation in the North China Craton (Taishan-Xintai area, western Shandong Province):Further evidence of an understated event from U-Pb dating and Hf isotopic composition of zircon. Precambrian Research,2011,186:169-180
Wang C Y, Zhang Q, Qian Q, et al. Geochemistry of the early Paleozoic Baiyin volcanic rocks (NW China):implications for the tectonic evolution of the North Qilian orogenic belt. The Journal of Geology.2005,113:83-94
Wang C, Jin Z M, Gao S, et al. Eclogite melt/peridotite reaction:Experimental constrains on the destruction mechanism of the North China Craton. SCIENCE CHINA Earth Sciences,2010,53:797-809
Wang F, Li X P, Chu H, Zhao G C. Petrology and metamorphism of khondalites from Jining Complex in the North China Craton. International Geology Review,2011,53:212-229
Wang H Z, Mo X X. An outline of the tectonic evolution of China. Episodes,1996:6-16
Wang S Y, Xu Z H, Pei S P. Velocity structure of uppermost mantle beneath China continent from Pn tomography. Science China:Earth Sciences,2002,45:143-150
Wang T, Guo L, Zheng Y D, et al. Timing and processes of late Mesozoic mid-lower-crustal extension in continental NE Asia and implications for the tectonic setting of the destruction of the North China Craton:Mainly constrained by zircon U-Pb ages from metamorphic core complexes. Lithos,2012,154:315-345
Wang X X, Wang T, Zhang C L. Neoproterozoic, Paleozoic, and Mesozoic granitoid magmatism in the Qinling Orogen, China:Constraints on orogenic process. Journal of Asian Earth Sciences,2013,72:129-151
Wilde S A, Cawood P A, Wang KY, et al. Granitoid evolution in the late Archean Wutai Complex, North China Craton. Journal of Asian Earth Sciences,2005,24:597-613
Wilde S A, Valley J W, Kita N T, et al. SHRIMP U-Pb and CAMECA1280oxygen isotope results from ancient detrital zircons in the Caozhuang quartzite, Eastern Hebei, North China Craton: evidence for crustal reworking3.8Ga ago. American Journal of Science,2008,308:185-199
Wilde S A, Zhao G C. Archean to Paleoproterozoic evolution of the North China Craton. Journal of Asian Earth Sciences,2005,24:519-522
Wilde S A, Zhao G C, Sun M. Development of the North China Craton during the Late Archaean and itsfinal amalgamation at1.8Ga; some speculations on its position within a global Palaeoproterozoic supercontinent. Gondwana Research,2002,5:85-94
Wilde S A, Zhao G C, Wang K Y, et al. First precise SHRIMP U-Pb zircon ages for the Hutuo Group, Wutaishan:further evidence for the Palaeoproterozoic amalgamation of the North China Craton. Chinese Science Bulletin,2004,49:83-90
Winchester J A, Floyd P A. Geochemical discrimination of different magma series and their differentiation products using immobile elements. Chemical Geology,1977,20:325-343
Winn R D. Large-scale traction produced structures in deep-water fan-channel conglomerates in southern chile. Geology,1977,5:41-44
Wu C L, Shi R D, Yang J S, et al. Petrogenesis and dating of two types of granite from North Qilian, China. Acta Geologica Sinica,2005,79:193-200
Wu Q F, Lu F X, Liu Q S, et al. Archean relic body at lower crust in Sulu area:Evidence from magnetic data. Chinese Science Bulletin,2003,48:589-593
Wynn R B, Stow D A V. Recognition and inter pretation of deep-water sediment waves: implications for palaeoceanography, hydrocarbon exploration and flow process in terpretation. Marine Geology,2002,192:1-3
Xia L Q, Xia Z C, Xu X Y. Magmagenesis in the Ordovician backarc basins of the North Qilian Mountains, China. GSA Bulletin,2003,115:1510-1522
Xia Q, Liu J, Liu S, et al. High water content in the Mesozoic lithospheric mantle of the North China Craton and implications for its destruction. Earth and Planetary Science Letters,2013,361:85-97
Xia X P, Sun M, Zhao G C, et al. LA-ICP-MS U-Pb geochronology of detrital zircons from the Jining Complex, North China Craton and its tectonic significance. Precambrian Research,2006b,144:199-212
Xia X P, Sun M, Zhao G C, et al. U-Pb and Hf isotopic study of detrital zircons from the Wulashan khondalites:Constraints on the evolution of the Ordos Terrane, Western Block of the North China Craton. Earth and Planetary Science Letters,2006a,241:581-593
Xia, X.P., Sun, M., Zhao, G.C., Wu, F.Y., Xu, P., Zhang, J.S. Paleoproterozoic crustal growth events in the Western Block of the North China Craton:Evidence from detrital zircon Hf and whole rock Sr-Nd isotopes of the khondalites in the Jining Complex. American Journal of Science,2008,308:304-327
Xie X Y, Heller P L. U-Pb detrital zircon geochronology and its implications:The early Late Triassic Yanchang Formation, south Ordos Basin, China. Journal of Asian Earth Sciences,2013,64:86-98
Xiong X L, Liu X C, Zhu Z M, et al. Adakitic rocks and destruction of the North China Craton: Evidence from experimental petrology and geochemistry. SCIENCE CHINA Earth Sciences,2011,54:858-870
Xu Y. Thermo-tectonic destruction of the Archaean lithospheric keel beneath the Sino-Korean Craton in China:Evidence, timing and mechanism. Phys Chem Earth,2001,26:747-757
Xu Y G, Li H Y, Pang C J, et al. On the timing and duration of the destruction of the North China Craton. Chinese Science Bulletin,2009,54, doi:10.1007/s11434-009-0346-5
Xue F, Kroner A, Reischmann T, et al. Palaeozoic pre-and post-collision calcalkaline magmatism in the Qinling orogenic belt, central China, as documented by zircon ages on granitoid rocks. Journal of the Geological Society,1996,153:409-417
Yang Y T, Li W, Ma L. Tectonic and stratigraphic controls of hydrocarbon systems in the Ordos Basin:a multicycle cratonic basin in central China. AAPG Bulletin,2005,89:255-269
Yang C H, Du L L, Ren L D, et al. Delineation of the ca.2.7Ga TTG gneisses in the Zanhuang Complex, North China Craton and its geological implications. Journal of Asian Earth Sciences,2013,72:178-189
Yang J H, Wu F Y, Wilde S A, et al. Mesozoic decratonization of the North China Block. Geology,2008,36:467-470
Yang Y T, Li W, Ma, L. Tectonic and stratigraphic controls of hydrocarbon systems in the Ordos basin:A multicycle cratonic basin in central China. AAPG Bulletin,2005,89:255-269
Yin C Q, Zhao G C, Guo J H, et al. U-Pb and Hf isotopic study of zircons of the Helanshan Complex:constrains on the evolution of the Khondalite Belt in the Western Block of the North China Craton. Lithos2011,122:25-38
Yin C Q, Zhao G C, Sun M, et al. LA-ICP-MS U-Pb zircon ages of the Qianlishan Complex: constrains on the evolution of the Khondalite Belt in the Western Block of the North China Craton. Precambrian Research,2009,174:78-94
Yuan W, Yang Z. The Alashan Terrane was not part of North China by the Late Devonian: Evidence from detrital zircon U-Pb geochronology and Hf isotopes, Gondwana Research,2014, http://dx.doi.Org/10.1016/j.gr.2013.12.009
Zeng H L, Xu D S, Tan H D. A model study for estimating optimum upward-continuation height for gravity separation with application to a Bouguer gravity anomaly over a mineral deposit, Jilin province, northeast China. Geophysics,2007,72(4):145-150
Zhai M G. Multi-stage crustal growth and cratonization of the North China Craton, Geoscience Frontiers,2014, doi:10.1016/j.gsf.2014.01.003
Zhai MG, Liu W J. Paleoproterozoic tentonic history of the North China Craton:A review. Precambrian Research,2003,122:183-199
Zhai M G, Bian A G, Zhao T P. The amalgamation of the supercontinent of North China Craton at the end of Neo～Archaean and its breakup during late Palaeoproterozoic and Mesoproterozoic. Science in China (Series D-Earth Science),2000,43:219-232
Zhai M G, Guo J H, Liu W J. Neoarchean to Paleoproterozoic continental evolution and tectonic history of the North China craton. Journal of Asian Earth Sciences,2005,24:547-561
Zhai M G, Liu W J. An oblique cross-section of Precambrian crust in the North China Craton. Physics and Chemistry of Earth (A),2001,26:781-792
Zhai M G, Santosh M. The early Precambrian odyssey of North China Craton:a synoptic overview. Gondwana Research,2011,20:6-25
Zhai M G, Shao JA, Hao J, et al. Geological signature and possible position of the North China block in the Supercontinent Rodinia. Gondwana Research,2003,6:171-183
Zhang C H, Li C M, Deng H L, et al. Mesozoic contraction deformation in the Yanshan and northern Taihang mountains and its implications to the destruction of the North China Craton. SCIENCE CHINA Earth Sciences,2011,54:798-822
Zhang C L, Liu L, Wang S J, et al. Detrital zircon provenance for the meta-sedimentary rocks from Kuanping Group, implicati on for Neo-proerozoic tectonic reconstruction in Qinling Orogeny, central China. In:Abstract with program of international discussion meeting on continental geology and tectonics. Northwest University Press, Xi'an,2009.64-66
Zhang H F. Destruction of ancient lower crust through magma underplating beneath Jiaodong Peninsula, North China Craton:U-Pb and Hf isotopic evidence from granulite xenoliths. Gondwana Research,2012a,21:281-292
Zhang H F, Sun M, Zhou X H, et al. Mesozoic lithosphere destruction beneath the North China Craton:Evidence from major, trace element and Sr-Nd-Pb isotope studies of Fangcheng basalts. Contributions to Mineralogy and Petrology,2002,144:241-254
Zhang H F, Ying J F, Santosh M, et al. Episodic growth of Precambrian lower crust beneath the North China Craton:A synthesis. Precambrian Research,2012a,222-223:255-264
Zhang H F, Zhu R X, Santosh M, et al. Episodic widespread magma underplating beneath the North China Craton in the Phanerozoic:Implications for craton destruction. Gondwana Research,2012b, doi:10.1016/j.gr.2011.1012.1006
Zhang J, Li J Y and Liu J F. Detrital zircon U-Pb ages of Early Paleozoic flysch sandstones in the western Ordos margin-New constrains on their provenances and rentonic implications. Journal of Asian Earth Sciences,2011,42:1030-1047
Zhang J F, Wang C, Wang Y F. Experimental constraints on the destruction mechanism of the North China Craton. Lithos,2012b,149:91-99
Zhang K J. Destruction of the North China Craton:Lithosphere folding-induced removal of lithospheric mantle? Journal of Geodynamics,2012b,53:8-17
Zhang Y B, Zhai M G, Lin Q, et al. Late Cretaceous volcanic rocks and associated granites in Gyeongsang Basin, SE Korea:Their chronological ages and tectonic implications for cratonic destruction of the North China Craton. Journal of Asian Earth Sciences,2012c,47:252-264
Zhao G C. Paleoproterozoic assembly of the North China Craton. Geology Magazine,2001,138:87-91
Zhao G C, Cawood P A. Precambrian Geology of China. Precambrian Research,2012,222-223:13-54
Zhao G C, Cawood P A, Wilde S A, et al. Metamorphism of basement rocks in the Central Zone of the North China Craton:implications for Paleoproterozoic tectonic evolution. Precambrian Research,2002,103:55-88
Zhao G C, Cawood P A, Wilde S A, et al. Amalgamation of the North China Craton:key issues and discussion. Precambrian Research,2012,222-223:55-76
Zhao G C, Kroner A, Wilde S A, et al. Lithotectonic elements and geological events in the Hengshan-Wutai-Fuping belt:a synthesis and implications for the evolution of the Trans-North China Orogen. Geological Magazine,2007,144:753-775
Zhao G C, Sun M, Wilde S A, et al. Late Archean to Paleoproterozoic evolution of the North China Craton:key issues revisited. Precambrian Research,2005,136:177-202
Zhao G C, Wilde S A, Cawood P A, et al. Thermal evolution of two textural types of mafic granulites in the North China Craton:evidence for both mantle plume and collisional tectonics. Geology Magazine,1999a,136:223-240
Zhao G C, Wilde S A, Cawood P A, et al. Tectonothermal history of the basement rocks in the western zone of the North China Craton and its tectonic implications. Tectonophysics1999b,310:37-53
Zhao G C, Wilde S A, Cawood P A, et al. Petrology and P-T-t path of the Fuping mafic granulites: implications for tectonic evolution of the central zone of the North China Craton. Journal of Metamorphic Petrology,2000,18:375-391
Zhao G C, Wilde S A, Cawood P A, et al. Archean blocks and their boundaries in the North China Craton:lithological, geochemical, structural and P-T path constraints and tectonic evolution. Precambrian Research,2001a,107:45-73
Zhao G C, Wilde S A, Cawood P A, et al. High-pressure granulites (retrograded eclogites) from the Hengshan Complex, North China Craton:petrology and tectonic implications. Journal of Petrology,2001b,42:1141-1170
Zhao G C, Wilde S A, Cawood P A, et al. Thermal evolution of basement rocks from the eastern part of the North China Craton and its bearing on tectonic setting. International Geology Reviews,1998,40:706-721
Zhao G C, Wilde S A, Zhang J. New evidence from seismic imaging for subduction during assembly of the North China craton:COMMENT. Geology,2010,38:206
Zhao G C, Zhai M G. Lithotectonic elements of Precambrian basement in the North China Craton: Review and tectonic implications. Gondwana Research,2013,23:1207-1240
Zheng J P, Griffin W L, Ma Q, et al. Accretion and reworking beneath the North China Craton. Lithos,2012,149:61-78
Zheng T Y, Zhao L, Zhu R X. New evidence from seismic imaging for subduction during assembly of the North China Craton. Geology,2009,37:395-398
Zheng Y F, Xiao W J, Zhao G C. Introduction to tectonics of China. Gondwana Research,2013,23:1189-1206
Zhou L H, Fu L X, Lou D, et al. Structural anatomy and dynamics of evolution of the Qikou Sag, Bohai Bay Basin:Implications for the destruction of North China craton. Journal of Asian Earth Sciences,2012,47:94-106
Zhu R X, Chen L, Wu F Y, et al. Timing, scale and mechanism ofthe destruction of the North China Craton. SCIENCE CHINA Earth Sciences,2011,54:789-797
Zhu Z Y, Jiang S Y, Liu G X, et al. Precise dating of the Middle Permian:Zircon U-Pb geochronology from volcanic ash beds in the basal Gufeng Formation, Yangtze region, South China. Gondwana Research,2013,23:1599-1606
Zhu G, Jiang D Z, Zhang B L, et al. Destruction of the eastern North China Craton in a backarc setting:Evidence from crustal deformation kinematics. Gondwana Research,2012a,22:86-103
Zhu R X, Xu Y G, Zhu G, et al. Destruction of the North China Craton. SCIENCE CHINA Earth Sciences,2012, doi:10.1007/s11430-012-4516-y
Zhu R X, Zheng T Y. Destruction geodynamics of the North China Craton and its Paleoproterozoic plate tectonics. Chinese Science Bulletin,2009,54, doi:10.1007/s11434-009-0451-5
安太庠,郑昭昌.鄂尔多斯盆地周缘的牙形石.北京：科学出版社,1990：12-132
柏冠军,吴汉宁,赵希刚,等.重力资料识别鄂尔多斯盆地线性构造方法研究.地球物理学进展,2007,22(5)：1386-1392
白斌,周立发,张义楷,等.贺兰山深部构造及其对浅部构造的响应过程.大地构造与成矿学,2008,32(1)：42-49
白瑾,黄学光,王惠初,等.中国前寒武纪地壳演化(第二版).北京：地质出版社,1996
白云来,王新民,刘化清,等.鄂尔多斯盆地西部边界的确定及其地球动力学背景.地质学报,2006,80(6)：792-813
包洪平,杨承运.鄂尔多斯东部奥陶系马家沟组微相分析.古地理学报,2000,2(1)：31-42
鲍志东,李儒峰,冯增昭.鄂尔多斯盆地东西部奥陶系对比再研究.地质论评,1999,45(4):375~381
蔡忠贤,蔡华,秦玉娟.鄂尔多斯盆地南缘早古生代碳酸盐岩高频沉积旋回分析.地球科学,1997,22(5):504~510
曹金舟,冯乔,赵伟,等.鄂尔多斯盆地南缘奥陶纪层序地层分析.沉积学报,2011,29:286~292
车自成,罗金海,刘良.中国及其邻区区域大地构造学(第二版).北京:科学出版社,2011.19~23,238~256
陈安清.鄂尔多斯地块早古生代盆地演化与物质聚集规律.博士学位论文.成都:成都理工大学,2010.1~137
陈诚,史晓颖,裴云鹏,等.鄂尔多斯盆地南缘晚奥陶世钾质斑脱岩SHRIMP测年及其成因环境.现代地质,2012,26(2):205~219
陈化奇.北祁连冷龙岭地区宁缠河花岗岩体的地球化学特征及大地构造意义.甘肃地质,2007,16:37~42
陈九辉,刘启元,李顺成等.青藏高原东北缘~鄂尔多斯地块地壳上地幔S波速度结构.地球物理学报,2005,48(2):333~342
陈凌,程骋,危自根.华北克拉通边界带区域深部结构的特征差异性及其构造意义.地球科学进展,2010,25(6):571~581
陈凌,危自根,程骋.从华北克拉通中、西部结构的区域差异性探讨克拉通破坏.地学前缘,2010,1:212~228
陈孟晋,汪泽成,郭彦如,等.鄂尔多斯盆地南部晚古生代沉积特征与天然气勘探潜力.石油勘探与开发,2006,33(1):1~5
陈明远.鄂尔多斯盆地北部地区重力资料的解释方法及其效果.石油与天然气地质,1988,9(4):325~333
陈孟晋,宁宁,胡国艺,等.鄂尔多斯盆地西部平凉组烃源岩特征及其影响因素.科学通报,2007,52(增刊Ⅰ):78~85
陈强,张慧元,李文厚,等.鄂尔多斯奥陶系碳酸盐岩碳氧同位素特征及其意义.古地理学报,2012,14(1):117~124
陈荣坤,孟祥化.华北地台早古生代沉积建造及台地演化.岩相古地理,1993,13(4):46~55.
传婷婷.鄂尔多斯盆地西缘奥陶系沉积特征及构造意义.硕士学位论文.北京:中国地质大学(北京),2013.1~65
崔智林,华洪,宋庆原.晚奥陶世北秦岭弧后盆地放射虫组合.地质学报,2000,74:254~259
邸领军,谢广成.对贺兰拗拉槽的质疑.岩性油气藏,2008,20(2):16~21,36
丁海军,孟祥化,葛铭,等.贺兰拗拉谷北段奥陶系等深流沉积.地球科学与环境学报,2009,31(1):58~65
丁海军,孟祥化,葛铭.米钵山组复理石中的内潮汐沉积.安徽地质,2008,18(4):241~247
丁燕云.鄂尔多斯盆地北部航磁反映的构造特征.物探与化探.2000,24(3):197~203
邓晋福,吴宗絮,赵国春,等.华北地台前寒武纪花岗岩类、陆壳演化与克拉通形成.岩石学报,1999,15:190~198
邓军,王庆飞,黄定华,等.鄂尔多斯盆地基底演化及其对盖层控制作用.地学前缘,2005,12(3):91~99
董春艳,万渝生,徐仲元,等.华北克拉通大青山地区古元古代晚期孔兹岩系:锆石SHRIMPU-Pb定年.中国科学:地球科学,2012,42:1851~1862
董兆雄,姚泾利,孙六一,等.重新认识鄂尔多斯南部早奥陶世马家沟期碳酸盐台地沉积模式.中国地质,2010,37(5):1327~335
董兆雄,赵敬松,方少仙,等.鄂尔多斯盆地南部奥陶纪末端变陡缓坡沉积模式.西南石油学院学报,2002,24:50~53
杜远生,朱杰,韩欣,等.从弧后盆地到前陆盆地~北祁连造山带奥陶纪~泥盆纪的沉积盆地与构造演化.地质通报,2004,23(9~10):911~917
杜远生,颜佳新,韩欣.造山带沉积地质学研究的新进展.地质科技情报,1995,14(1):29~34
杜远生,朱杰,顾松竹,等.北祁连造山带寒武系~奥陶系硅质岩沉积地球化学特征及其对多岛洋的启示.中国科学:地球科学,2007,37(10):1314~1329
方迎尧,张培琴,刘浩军.低磁纬度地区ΔT异常解释的途径与方法.物探与化探,2006,30(1):48
费安玮,刘成林,甘军,等.鄂尔多斯盆地三道坎组混合沉积的生物扰动构造与古地理.中国地质,2004,31(4):347~355
费安玮,张忠涛.陕西金粟山中奥陶统生物扰动构造与古环境分析.地球科学,2002,27(6):703~710
冯益民,何世平.祁连山及其邻区大地构造基本特征~兼论早古生代海相火山岩的成因环境.西北地质科学,1995,16:92~103
冯益民,何世平.祁连山大地构造与造山作用.北京:地质出版社,1996:1~135.
冯增昭,鲍志东,康祺发,等.鄂尔多斯早古生代古地理.1999b,1,84~91
冯增昭,鲍志东,康祺法,等.鄂尔多斯早古生代古构造.古地理学报,1999,1(2):84~91.
冯增昭,鲍志东,张永生.鄂尔多斯奥陶纪地层岩石岩相古地理.北京:地质出版社,1998.1~144
冯增昭,鲍志东.鄂尔多斯奥陶纪马家沟期岩相古地理.沉积学报,1999a,17,1~8
付金华,郑聪斌.鄂尔多斯盆地奥陶纪华北海和祁连海演变及岩相古地理特征.古地理学报,2001,3(4):25~34
高振中,何幼斌,李向东.中国地层记录中的内波及内潮汐沉积研究.古地理学报,2010,12(5):527~534
高振中,何幼斌,刘成鑫,等.深水牵引流沉积的研究历程、现状与前景.古地理学报,2006,8(3):331~338
高振中,何幼斌,罗顺社,等著.深水牵引流沉积~内潮汐、内波和等深流沉积研究.北京:科学出版社,1996,1~112
高振中,何幼斌,张兴阳,等.塔中地区中晚奥陶世内波、内潮汐沉积.沉积学报,2000,18(3):400~407
高振中,罗顺社,何幼斌,等.鄂尔多斯地区西缘中奥陶世等深流沉积.沉积学报,1995b,13(4):16~26
高振中,罗顺社,何幼斌,等.鄂尔多斯西缘奥陶纪海底扇沉积体系.石油与天然气地质,1995a,16(2):119~126
葛梅钰,郑昭昌,李玉珍.宁夏及其邻近地区奥陶纪、志留纪笔石地层及笔石群.南京:南京大学出版社,1990,1~190
葛文春,吴福元,周长勇,等.大兴安岭北部塔河花岗岩体的时代及对额尔古纳地块构造归属的制约.科学通报,2005,50:1239~1247
耿建珍,张健,李怀坤,等.10μm尺度锆石U~Pb年龄的LA~MC~ICP~MS测定.地球学报,2012,33:877~884
耿元生,沈其韩,任留东.华北克拉通晚太古代末~古元古代初的岩浆事件及构造热体制.岩石学报,2010,26:1945~1966
管志宁,安玉林,吴朝钧.磁性界面反演及华北地区深部构造的推断.见:王懋基,程家印主编.
勘查地球物理勘查地球化学文集(第6集),中国区域地球物理研究.北京:地质出版社.1987,802~101
郭慧丽,徐佩芬.地震层析成像在华北克拉通地区的研究进展.地球物理学进展,2011,26(5):1557~1565
郭飚,刘启元,陈九辉,等.青藏高原东北缘~鄂尔多斯地壳上地幔地震层析成像研究.地球物理学报,2004,47(5):790~797
郭峰,郭岭,赵卫卫.贺兰坳拉谷奥陶纪岩相古地理．海相地质与第四纪地质,2011,31(5):51~58
郭锋,范蔚茗,李超文,等.早古生代古亚洲洋俯冲作用:来自内蒙古大石寨玄武岩的年代学与地球化学证据.中国科学D辑:地球科学,2009,39:569~579
郭建秋,张雄华,章泽军.江西修水地区中元古界双桥山群修水组内波内潮汐沉积.地质科技情报,2003,22(1):47~52
郭建秋,张雄华,章泽军,等.赣西北前寒武系首次发现内波内潮汐沉积.地质科学,2004,39(3):329~338
郭彦如,赵振宇,付金华,等.鄂尔多斯盆地奥陶纪层序岩相古地理.石油学报,2012,33(增刊2):95~109
郭依群,王嘹亮,匡增桂,等.等深流沉积特征.海洋地质前沿,2012,28(6):1~9
韩品龙,张月巧,冯乔.鄂尔多斯盆地祁连海域奥陶纪岩相古地理特征及演化.现代地质,2009,22:822~827
何幼斌,高振中,郭成贤,等.石门杨家坪下寒武统杷榔组三段内波和内潮汐沉积研究.中国地质,2005,32(1):62~69
何幼斌,高振中,李建明,等.浙江桐庐晚奥陶世内潮汐沉积.沉积学报,1998,16(1):1~7
何幼斌,高振中,张兴阳,等.塔里木盆地塔中32井中上奥陶统内潮汐沉积.古地理学报,2003,5(4):414~425
何幼斌,罗顺社,高振中.内波、内潮汐沉积研究现状与进展.江汉石油学院学报,2004,26(1):5~11
何幼斌,高振中,罗顺社,等.陕西陇县地区平凉组三段发现内潮汐沉积.石油天然气学报,2007,29(4):28~33
何自新,杨华,袁效奇.鄂尔多斯盆地地质剖面图集.北京:石油工业出版社,2004.1~422
何自新.鄂尔多斯盆地演化与油气.北京:石油工业出版社,2003:22~31
侯方浩,方少仙,赵敬松；等.鄂尔多斯盆地中奥陶统马家沟组沉积环境模式.海相油气地质,2002,7(1):38~46
侯方浩,方少仙,董兆雄,等.鄂尔多斯盆地中奥陶统马家沟组沉积环境与岩相发育特征.沉积学报,2003,21:106~112
胡波,翟明国,彭澎,等.华北克拉通古元古代末~新元古代地质事件-来自北京西山地区寒武系和侏罗系碎屑锆石LA~ICP~MSU~Pb年代学的证据.岩石学报,2013,29:2508~2536
胡波,翟明国,郭敬辉,等.华北克拉通北缘化德群中碎屑锆石的LA-ICP-MSU-Pb年龄及其构造意义.岩石学报,2009,25(1):193~211
胡晓,许传诗,牛树根.华北地台北缘早古生代大陆边缘演化.北京:北京大学出版社,1990,1~185
胡艳华,刘健,周明忠,等.奥陶纪和志留纪钾质斑脱岩研究评述.地球化学,2009,38,393~404
黄汲清.中国大地构造特征的新研究.中国地质科学院院报,1984,9:5~20
黄汲清等.中国大地构造及其演化.北京:科学出版社,1980
黄汲清,任纪舜,姜春发,等.中国大地构造基本轮廓.地质学报,1977,52(2):117~135黄喜峰,钱壮志,逯东霞,等.贺兰山中南段奥陶系米钵山组的沉积环境与构造背景分析.地球学报,2009,30(1):65~71
黄喜峰,钱壮志,孙保平,等.北祁连造山带与贺兰冷裂谷构造边界的探讨.桂林理工大学学报,2010,30(2):195~201
嵇少丞,王茜,许志琴.华北克拉通破坏与岩石圈减薄.地质学报,2008,82(2):174~193
贾进斗,何国琦,李茂松,等.鄂尔多斯盆地基底结构特征及其对古生界天然气的控制.高校地质学报,1997,3(2):144~153
嘉世旭,张先康.华北不同构造块体地壳结构及其对比研究.地球物理学报,2005,48:611~620
贾振远,蔡华,蔡忠贤,等．鄂尔多斯地区南缘奥陶纪层序地层及海平面变化．地球科学~中国地质大学学报,1997,22:491~503
贾振远.一个碳酸盐沉积古斜坡的基本特征.石油与天然气地质,1988,9:171~178
江为为,郝天珧,宋海斌.鄂尔多斯盆地地质地球物理场特征与地壳结构.地球物理学进展,2000,15(3):45~53
晋慧娟,李育慈,方国庆.西秦岭古代地层记录中内波、内潮汐沉积及其成因解释.沉积学报,2002,20(1):80~84
晋慧娟,李育慈,方国庆.中国古代深海沉积和遗迹化石群落.科学出版社,2003:1~231
晋慧娟,李育慈.深海沉积中的几种“特殊”原生沉积构造.中国科学(B辑),1998,25(8):890~896
晋慧娟,孙明良,李育慈.内蒙古桌子山中奥陶统的“特殊”浊积岩系.沉积学报,2005,23(1):34~40
李安仁,刘文均,张锦泉,等.鄂尔多斯盆地早奥陶世沉积特征及其演化.成都地质学院学报,1993,20(1):17~26
李斌,史晓颖,程长青,等.空间数据库技术在定量单因素作图法中的应用-以鄂尔多斯盆地奥陶系SQ17岩相古地理研究为例.煤田地质与勘探,2010,38(1):1~6
李春昱,王荃,张之孟,等.中国板块构造的轮廓.中国地质科学院院报,1980,2(1):11~20
李怀坤,耿建珍,郝爽,等.用激光烧蚀多接收器等离子体质谱仪(LA-MC-ICPMS)测定锆石U-Pb同位素年龄的研究.矿物岩石地球化学通报,2009b,28(增刊):77
李怀坤,陆松年,李惠民,等.侵入下马岭组的基性岩床的锆石和斜锆石U-Pb精确定年-对华北中元古界地层划分方案的制约.地质通报,2009a,28:1396~1404
李怀坤,苏文博,周红英,等.华北克拉通北部长城系底界年龄小于1670Ma-来自北京密云花岗斑岩岩脉锆石LA-MC-ICPMSU-Pb年龄的约束.地学前缘,2011,18:108~120
李怀坤,朱士兴,相振群,等.北京延庆高于庄组钾质斑脱岩的锆石U~Pb定年研究及其对华北北部中元古界划分新方案的进一步约束.岩石学报,2010,26:2131~2140
李建明,何幼斌,高振中,等.湖南桃江半边山前寒武纪内潮汐沉积及其共生沉积特征.石油天然气学报(江汉石油学院学报),2005b,27(5):545~547
李建明,王华,何幼斌,等.浙江临安上奥陶统复理石中的内潮汐沉积.石油天然气学报(江汉石油学院学报),2005a,27(1):1~4
李明瑞.鄂尔多斯盆地北部上古生界主要含气砂体沉积特征及储层控制因素研究.博士学位论文.成都:成都理工大学,2011.1~186
李少华,王彦宾,梁子斌,等.甘肃东南部地壳速度结构的区域地震波形反演.地球物理学报,2012,55(4):1186~1197
李文厚,陈强,李智超,等.鄂尔多斯地区早古生代岩相古地理.古地理学报,2012,14:85~100
李文厚,梅志超,陈景维,等.陕西渭北奥陶系放射虫硅质岩与火山钾质斑脱岩的成因环境.中国区域地质,1997,16:422~427
李祥辉,王成善,胡修棉.深海相中的砂质碎屑流沉积~以西藏特提斯喜马拉雅侏罗~白垩系为例.矿物岩石,2000,20(1):45~51
李向东,何幼斌,王丹,等.贺兰山以南中奥陶统香山群徐家圈组古水流分析.地质论评,2009a,55(5):653~662
李向东,何幼斌,王丹,等.宁夏中奥陶统香山群徐家圈组内波和内潮汐沉积.古地理学报,2009b,11(5):513~523
李向东,何幼斌,张铭记,等.宁夏中奥陶统香山群徐家圈组内波、内潮汐沉积类型.地球科学进展,2011,26(9):1006~1014
林畅松,杨起,李思田,等.贺兰奥拉槽早古生代深水重力流体系的沉积特征和充填样式.现代地质,1991,5(3):252~262
林畅松,杨起,李思田.贺兰拗拉槽盆地充填演化分析.北京:地质出版社,1995
刘宝宪,闫小雄,白海峰,等.鄂尔多斯盆地南缘中奥陶统平凉组成藏条件分析.天然气地球科学,2008,19:657~661
刘成鑫,高振中,纪友亮,等.鄂尔多斯盆地西南缘奥陶系深水牵引流沉积.海洋地质与第四纪地质,2005,25(2):31~36
刘德汉,付金华,郑聪斌,等.鄂尔多斯盆地奥陶系海相碳酸盐岩生烃性能与中部长庆气田气源成因研究.地质学报,2004,4:542~550
刘敦一,简平,张旗,等.内蒙古图林凯蛇绿岩中埃达克岩SHRIMP测年:早古生代洋壳消减的证据.地质学报,2003,77:317~327
刘浩军,薛典军,郭志宏,等.航空物探软件系统研制.物探与化探,2003,27(2):146~149
刘军锋,孙勇,孙卫东.秦岭拉鸡庙镁铁质岩体锆石LA~ICP~MS年代学研究.岩石学报,2009,25(2):320~330
刘钦甫,杨晓杰,丁述理.华北晚古生代煤系高岭岩微量元素和稀土元素地球化学研究.地球化学,1998,27(2):196~203
刘振军,张永军,赵百民.分带变倾角化极磁场图在大范围航磁解释中的应用.物探与化探,2010,34(2):221~224
马昌前,明厚利,杨坤光.大别山北麓的奥陶纪岩浆弧:侵入岩年代学和地球化学证据.岩石学报,2004,20:393~402
马杏垣,吴正文,谭应佳,等.华北地台基底构造.地质学报,1979,4:293~304
毛光周,刘池洋.地球化学在物源及沉积背景分析中的应用.地球科学与环境学报,2011,33(4):337~349
梅志超,陈景维,卢焕勇,等.陕西富平中奥陶统平凉组的深水碳酸盐碎屑流.石油与天然气地质,1982,3:49~56
孟祥化,葛铭.中朝板块层序·事件·演化.北京:科学出版社,2004:1~516
苗来成,刘敦一,张福勤,等.大兴安岭韩家园子和新林地区兴华渡口群和扎兰屯群锆石SHRIMPU-Pb年龄.科学通报,2007,52:591~601
宁夏回族自治区地质矿产局.宁夏回族自治区区域地质志.北京:地质出版社,1990:1~522
宁夏回族自治区地质矿产局.宁夏回族自治区岩石地层．武汉:中国地质大学出版社,1996:1~132
庞雄,陈长民,朱明,等.深水沉积研究前缘问题.地质论评,2007,53(1):36~43
裴福萍,许文良,杨德彬,等.松辽盆地基底变质岩中锆石U-Pb年代学及其地质意义.科学通报,2006,51:2882~2891
彭澎,翟明国.华北陆块前寒武纪两次重大地质事件的特征和性质.地球科学进展,2002,17:818~825
钱锋,艾永峰.鄂尔多斯南部地区早古生代主动大陆边缘演化特征.西安工程学院学报,2002,24:18~24
乔秀夫,张安棣.华北块体、胶辽朝块体与郯庐断裂.中国地质,2002,29(4):337~345
秦海鹏.北祁连造山带早古生代花岗岩岩石学特征及其与构造演化的关系.博士学位论文.北京:中国地质科学院,2012.1~141
屈红军,梅志超,李文厚,等.陕西富平地区中奥陶统等深流沉积的特征及其地质意义.地质通报,2010,29(9):1304~1309
阮小敏,孙若昧,滕吉文,等.鄂尔多斯及其周边地区地壳上地幔地震层析成像研究.中国地球物理学会第二十五届年会,2009,368
任纪舜等.中国东部及邻区大陆岩石圈的构造演化与成矿.北京:科学出版社,1990
ShanmugamG.深水砂体成因研究新进展.石油勘探与开发,2013c,40(3):294~301
陕西省地质矿产局.陕西省区域地质志.地质出版社,1989.1~698
陕西省地质矿产局.陕西省岩石地层.武汉:中国地质大学出版社,1998.1~291
施光海,刘敦一,张福勤,等.中国内蒙古锡林郭勒杂岩SHRIMP锆石U~Pb年代学及意义.科学通报,2003,48:2187~2192
史基安,邵毅,张顺存,等.鄂尔多斯盆地东部地区奥陶系马家沟组沉积环境与岩相古地理研究.天然气地球科学,2009,20(3):316~324
石玉若,刘敦一,张旗,等.内蒙古苏左旗地区闪长~花岗岩类SHRIMP年代学.地质学报,2004,78:789~799
宋凯,吕剑文,杜金良,等.鄂尔多斯盆地中部上三叠统延长组物源方向分析与三角洲沉积体系.古地理学报,2002,4(3):59~66
宋述光,张立飞,Y.Niu,等.北祁连山榴辉岩锆石SHRIMP定年及其构造意义.科学通报,2004,49:592~595
宋述光.北祁连山古大洋俯冲带高压变质岩研究评述.地质通报,2009,28:1769~1778
苏文博,李志明,EttensohnFR,JohnsonME,etal.华南五峰组-龙马溪组黑色岩系时空展布的主控因素及其启示.地球科学,2007,32(6):819~827
苏文博,李志明,史晓颖,等.华南五峰组-龙马溪组与华北下马岭组的钾质班脱岩及黑色岩系-两个地史转折期板块构造运动的沉积响应.地学前缘,2006,13(6):82~95
苏文博,何龙清,王永标,等.华南奥陶-志留系五峰组及龙马溪组底部斑脱岩与高分辨综合地层.中国科学D辑,2002(3):207~219
孙国凡,刘景平.贺兰坳拉槽与前渊盆地及其演化.石油与天然气地质,1983,4(3):236~245.
孙国凡,谢秋元，刘景平等.鄂尔多斯盆地的演化盈加与含油气性.石油与天然气地质,1986，7(4):356~366
孙晓猛,张旗,钱青.甘肃肃南白泉门地区蛇绿混杂岩地质特征.地球科学进展,1997,12(40):340~350
孙肇才,胡显穆.鄂尔多斯盆地西南缘奥陶系的对比划分意见及其对中西部油气勘探的意义.海相油气地质,2002,7:41~58
孙肇才,谢秋元.叠合盆地的发展特征及其含油气性—以鄂尔多斯盆地为例.石油实验地质,1980,1:3~21
滕吉文,王夫运,赵文智,等.鄂尔多斯盆地上地壳速度分布与沉积建造和结晶基底起伏的构造研究.地球物理学报,2008,51(6):1753~1766
王昌勇,郑荣才,王海红,等.鄂尔多斯盆地姬塬地区长6油层组物源区分析.沉积学报,2008,26(6):933~938
王官福,张文治.华北陆台北缘重磁异常的地质解释.物探与化探,1992,16:31~37
王国茹,陈洪德,朱志军,等.川东南~湘西地区志留系小河坝组砂岩稀土元素特征及其地质意义.石油实验地质,2010,32(5):487~495
王宏伟,何幼斌,孙宜显.甘肃夏河上二叠统内波、内潮汐沉积.石油天然气学报(江汉石油学院学报),2005,27(s4):561~562
王鸿祯.中国古地理图集.北京:地图出版社,1985:37~46
王鸿祯,何国琦,张世红.中国与蒙古之地质.地学前缘,2006,13(6):1~13
王鸿祯,刘本培,李思田.中国及邻区大地构造划分和构造发展阶段.见:王鸿祯,杨森楠,刘本培等著.中国及邻区构造古地理和生物古地理.武汉:中国地质大学出版社,1990:3~34
王鸿祯,莫宣学.中国地质构造述要.中国地质,1996:4~9
王鸿祯,杨森楠,李思田.中国东部及邻区中、新生代盆地发育及大陆边缘区的构造发展.地质学报,1983,3:213~223
王廷印,高军平,王金荣,等.内蒙古阿拉善北部地区碰撞期和后造山期岩浆作用.地质学报,1998,72(2):126~137
王涛,徐鸣洁,王良书,等.鄂尔多斯及邻区航磁异常特征及其大地构造意义.地球物理学报,2007,50:163~170
王志铄,王椿镛,曾融生,等.华北及邻区地壳上地幔三维速度结构的地震走时层析成像.CT理论与应用研究,2008,17(2):15~27
王少昌,付琐堂,李熙哲,等.鄂尔多斯盆地西缘古生代槽台过渡带裂谷系弧形构造带的形成与发展及对油气聚集富集规律的影响.天然气地球科学,2005,16(4):421~427
王同和.晋陕地区地质构造演化与油气聚集.华北地质矿产杂志,1995,10(3):283~398
王学平.鄂尔多斯南缘奥陶纪地层对比分析.陕西地质,2002,20:20~26
王玉新.鄂尔多斯地块早古生代构造格局及演化.地球科学:中国地质大学学报,1994,19(6):778~786
王振涛,周洪瑞,王训练,等.贺兰山地区中奥陶统樱桃沟组物源及构造背景分析.沉积学报,2014,32(2):205~217
魏魁生等著.碳酸盐岩层序地层学~以鄂尔多斯盆地为例.北京:地质出版社,2000,1~135
魏文博,金胜,叶高峰,等.华北地区大地电磁测深及岩石圈厚度讨论.中国地质,2006,33(4):762~772
吴胜和,冯增昭,张吉森.鄂尔多斯地区西缘及南缘中奥陶统平凉组重力流沉积.石油与天然气地质,1994,15(3):226~235
席胜利,郑聪斌,李振宏.鄂尔多斯盆地西缘奥陶系地球化学特征及其沉积环境意义.古地理学报,2004,6(2):196~206
夏林圻,夏祖春,徐学义.北祁连山奥陶纪弧后盆地火山岩浆成因.中国地质,2003,30(1):48~60
夏林圻,夏祖春,徐学义.北祁连山构造~火山~岩浆演化动力学.西北地质科学,1995,16:1~28
夏林圻,夏祖春,徐学义.北祁连山早古生代洋脊~洋岛和弧后盆地火山作用.地质学报,1998,72(4):301~312
夏明军,郑聪斌,毕建霞,等.鄂尔多斯盆地奥陶系生物礁及其天然气勘探前景.天然气地球科学,2008,19(2):178~182,271
辛勇光,周进高,邓红婴.鄂尔多斯盆地南部下奥陶统马家沟组沉积特征.海相油气地质,2010,15(4):1~5
许强,陈洪德,赵俊兴等.贺兰拗拉槽胡基台地区中奥陶统樱桃沟组深海重力流沉积特征.海相油气地质,2010,15(2):14~20
薛春纪,池国祥,薛伟,等.鄂尔多斯盆地生烃过程与流体流动及铀矿化关系.地学前缘,2011,18(5):19~28
许文彬,徐茂泉,孙美琴.等深流沉积研究现状与展望.台湾海峡,2004,23(3):394~402
许效松,徐强,潘桂棠,等.中国南大陆演化与全球古地理对比.北京:地质出版社,1996
许志琴,杨经绥,李海兵,姚建新.中央造山带早古生代地体构架与高压/超高压变质带的形成.地质学报,2006,80(12):1793~1805
闫全人,王宗起,闫臻,等.从华北陆块南缘大洋扩张到北秦岭造山带板块俯冲的转换时限.地质学报,2009,83:1565~1583
杨华,付金华,包洪平.鄂尔多斯地区西部和南部奥陶纪海槽边缘沉积特征与天然气成藏潜
力分析.海相油气地质,2010,15(2):1~13
杨江海,杜远生,朱杰.甘肃景泰崔家墩下奥陶统阴沟组砂岩化学组分特征及物源区构造背景判别.古地理学报,2007,9(2):197~206
杨江海.造山带碰撞~隆升过程的碎屑沉积响应:以北祁连志留系、右江二叠~三叠系和大别山南麓侏罗系为例.博士学位论文.武汉:中国地质大学(武汉),2012.1~151
杨俊杰,张伯荣.陕甘宁盆地油气区及油气藏序列.石油学报,1988,9(1):1~8
杨俊杰著.鄂尔多斯盆地构造演化与油气分布规律.北京:石油工业出版社,2002:1~85
杨森楠,姜本鸿,王祖春.华北与扬子陆块碰撞带构造古地理的特征和发展.见:王鸿祯,杨
森楠,刘本培等著.中国及邻区构造古地理和生物古地理.武汉:中国地质大学出版社,1990:165~186
杨遂正,金文化,李振宏.鄂尔多斯多旋回叠合盆地形成与演化.天然气地球科学,2006,17(4):494~498
杨婷,吴建平,房立华,等.华北地区地壳上地幔S波三维速度结构.地球物理学进展,2012,27(2):441~454
杨文敬.鄂尔多斯西缘奥陶纪沉积演化及其控制下的油气地质条件.硕士学位论文.西安:西北大学,2006.1~81
殷洪福,黄思骥,张克信,等.华南二叠纪~三叠纪之交的火山活动及其对生物灭绝的影响.地质学报,1989,63(2):169~180
袁鹤然,郑绵平,陈文西,张永生,等.陕北成盐盆地奥陶纪成钾找钾远景分析.地质学报,2010,84(11):1554~1564
袁卫国,赵一鸣.鄂尔多斯南部地区早古生代被动大陆边缘特征与演化.西北大学学报(自然科学版),1996,26:451~454
袁卫国．鄂尔多斯盆地南缘中奥陶统火山钾质斑脱岩的研究与意义.石油实验地质,1995,17:167~170
袁效奇,耿国仓.巴彦浩特盆地东部古生代沉积的发现及其大地构造意义.石油与天然气地质,1992,13(4):381~389
袁照令,李大明.关于磁异常化到地磁极问题的几点认识.物探化探计算技术,1998,20(3):284
翟明国.华北克拉通的形成演化与成矿作用.矿床地质,2010,29:24~36
翟明国.华北克拉通中生代破坏前的岩石圈地幔与下地壳.岩石学报,2008,24(10):2185~2204
张福礼.鄂尔多斯盆地早古生代复合的古构造体系与天然气.地质力学学报,2002,8(3):193~2000张泓,白清昭,张笑微,等.鄂尔多斯聚煤盆地形成与演化.西安:陕西科学技术出版社,1995
张进,李锦轶,刘建峰,等.早古生代阿拉善地块与华北地块之间的关系:来自阿拉善东缘中奥陶统碎屑锆石的信息.岩石学报,2012,28(9):2912~2934
张进,马宗晋,任文军.再论贺兰山地区新生代之前拉张活动的性质.石油学报,2004,25:8~11张抗.鄂尔多斯断块构造和资源.西安:陕西科学技术出版社,1989:7~8,29~81,193~250
张抗.鄂尔多斯断块太古代至早元古代构造发育特征.地质科学,1982:352~363
张抗.鄂尔多斯盆地西、南缘奥陶系滑塌堆积.沉积学报,1992,10(1):11~18
张抗.论贺兰裂堑.见:鄂尔多斯盆地西缘地区石油地质论文集.呼和浩特:内蒙古人民出版社,1983:29~40
张旗,孙晓猛,周德进,等.北祁连蛇绿岩特征、形成环境及其构造意义.地球科学进展,1997a,12(4):366~393
张旗,王岳明,钱青,等.甘肃景泰县老虎山地区蛇绿岩及其上覆岩系中枕状熔岩的地球化学特征.岩石学报,1997,13:92~99
张道峰,杨文敬,漆亚玲,等.鄂尔多斯盆地神木地区上古生界山西组物源分析.天然气地球科学,2009,20(6):902~906
章贵松,张军,任军峰,等.六盘山弧形冲断体系构造新认识.新疆石油地质,2006,27(5):542~544
张国伟,张本仁,袁学诚,等.秦岭造山带与大陆动力学.北京:科学出版社,2001
张吉森,费安琦,王志辉.鄂尔多斯西、南部中奥陶世环陆架沉积特征.石油与天然气地质,1982,3(4):360~368
张家声,李燕,黄雄南.中国北部古元古代地壳尺度的伸展拆离和硅铝壳内活动带:北东向线性航磁异常的地质构造解释.地质科学,2007,42:267~302
张家声,索书田.华北北部结晶基底中的大型韧性剪切带.中国区域地质,1988(4),289~296
张建新,许志琴,陈文,等.北祁连中段俯冲~增生杂岩/火山弧的时代探讨.岩石矿物杂志,1997,16:112~119
张金川.鄂尔多斯盆地构造演化及含油气展望.天然气地质,1982,3(4):304~315
张俊明,李国祥,周传明.滇东下寒武统含磷岩系底部火山喷发事件沉积及其意义.地层学杂志,1997,21(2):91~99,155
张俊明,李国祥,周传明.滇东早寒武世梅树村期浅角粘土岩层的地球化学特征和地质意义.岩石学报,1997,13(1):100~110
张培琴,赵群友.低磁纬度区航磁异常变倾角磁方向转换方法.物探化探计算技术,1996,18(3):206
张勤文,徐道一.地层界线上灾变事件标志和成因的探讨.地球学报,1994,15(3/4):192~199
张锡林,姚长利.低磁纬度地区磁异常化极方法及应用.石油物探,2003,42(4):541
张先,李长法,贺为民.鄂尔多斯北缘地震带地壳磁性层特征.见:中国地球物理学会第七届学术年会论文集,1991
张永军,张开均.根据航磁数据探讨阿尔金断裂带的结构及构造演化.物探与化探,2007,31(6):489~494
赵国春.华北克拉通基底主要构造单元变质作用及其若干问题讨论.岩石学报,2009,25(8):1172~1792
赵国泽,詹艳,王立凤,等.鄂尔多斯断块地壳电性结构.地震地质,2010,32(3)345~359
赵红格,刘池洋,王峰,等.鄂尔多斯盆地西缘构造分区及其特征.石油与天然气地质,2006,27(2):173~179
赵振宇,郭彦如,王艳,等.鄂尔多斯盆地构造演化及古地理特征研究进展.特种油气田,2012,19(5):15~20
赵重远.鄂尔多斯地块西缘构造演化及板块应力机制分析.见:鄂尔多斯盆地西缘地区石油地质论文集.呼和浩特:内蒙人民出版社,1983:20~28
赵宗溥,等.中朝准地台前寒武纪地壳演化.北京:科学出版社,1993.366~388
郑绵平,齐文,张永生.中国钾盐地质资源现状与找钾方向初步分析.地质通报,2006a,5(11):1239~1246
郑绵平,袁鹤然,赵希涛,等.青藏高原第四纪泛湖期与古气候.地质学报,2006b,80(2):169~180
郑绵平,袁鹤然,张永生,等.中国钾盐区域分布与找钾远景.地质学报,2010,84(11):1523~1553
郑昭昌,李玉珍.贺兰山奥陶系研究的新进展.现代地质,1991,6(5):119~137
《中国石油天然气的勘查与发现》编辑部.中国石油天然气的勘查与发现.北京:地质出版社,1992
周安朝.华北地块北缘晚古生代盆地演化及盆山耦合关系.博士学位论文.西安:西北大学,2000.1~144
周立宏,李三忠,刘建忠,等.渤海湾盆地区燕山期构造特征与原型盆地.地球物理学进展,2003,18(4):692~699
周书昌,冯乔,赵伟,等.鄂尔多斯盆地南缘岐山剖面中奥陶统平凉组沉积环境分析.沉积与特提斯地质,2011,31:28~33
周进高,张帆,郭庆新,等.鄂尔多斯盆地下奥陶统马家沟组障壁潟湖沉积相模式及有利储层分布规律.沉积学报,2011,29(1):64~71
周民都,王椿镛,曾融生.青藏高原东北缘地壳上地幔速度结构的地震层析成像研究.西北地震学报,2012,34(3):224~233
周喜文,赵国春,耿元生.贺兰山高压泥质麻粒岩-华北克拉通西部陆块拼合的岩石学证据.岩石学报,2010,26(7),2113~2121
朱光,胡召齐,陈印,等.华北克拉通东部早白垩世伸展盆地的发育过程及其对克拉通破坏的指示.地质通报,2008,27(17):1594~1604
朱如凯,孟祥化,葛铭.巴彦浩特盆地东缘中奥陶统混合型深水重力流沉积层序及其旋回.沉积学报,1994,12(2):77~85
左朝国,刘义科,张崇.北祁连造山带中-西段陆壳残块群的构造-地层特征.地质科学,2002,37:302~312
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |