贺兰山地区中晚三叠世物源分析及其时空演化过程
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摘要
系统分析物源的时空演化过程,必将为判断当时的盆地构造背景和盆地属性提供佐证。文中运用重矿物分析方法,结合砾石岩性组成、地层厚度变化及沉积相分布规律,对贺兰山地区中晚三叠世沉积物源进行系统分析。结果表明:贺兰山地区中晚三叠世沉积物具有多源、混源以及上下层段时空演化差异明显的特点。中三叠世纸坊期物源主要来自盆地西北部和西部;晚三叠世延长期T3y1、T3y2段沉积时期,物源主要来自盆地西北部、西部、南部; T3y3至T3y5段沉积时期,盆地东部物源开始出现,并分布于贺兰山汝箕沟沟口至鬼头沟一线,此时汝箕沟—香棒子沟一带是沉积混源中心。西部物源主要为阿拉善地块之上的沉积地层,但西部南段受南部物源控制,与西部北段的物源岩性有较明显不同;西北部物源主要是孔兹岩带、前寒武纪变质岩及古生代岩浆岩;东部地区物源可能为现今银川地堑及其东部的沉积地层。贺兰山地区中晚三叠世物源时空演化的转折期,主要在纸坊期至延长期T3y1段沉积时期之间和延长期T3y2段至T3y3段沉积时期之间,2次明显的物源演化反映了贺兰山盆地构造动力学机制的重大转变。
Combined with conglomerate composition,strata thickness and sedimentary facies,heavymineral compositions were firstly used to study the provenances of the Middle-Late Triassic in the Helan Mountain. Results showed that the provenance of the Middle-Late Triassic sediments in the Helan Mountain were characterized by multiple and mixed sources,and were varied greatly. Sediments of the Middle Triassic Zhifang Formation were mainly from northwest and west. However,sediments of the Late Triassic Yanchang Formation changed. During deposition of the lower two members T3 y1 and T3 y2,sediments were mainly derived from the northwest,west and south. During deposition of the upper three members T3 y3 to T3 y5,eastern sources appeared,which were distributed in the Ruqigou to Xiangbangzigou. The western provenance was mainly in the sedimentary strata on the Alxa Block. Sediments of northwestern part were mainly from the Precambrian metamorphic rocks and Paleozoic magmatic rocks in the Paleoproterozoic Khondalite Belt,which was different from the southwestern part. Sediments in its eastern part were sourced from the sedimentary strata of Yinchuan graben and areas to its east. Provenance transformation of the Middle-Late Triassic strata in the Helan basin occurred twice: One from the Zhifang to Yanchang formations T3 y1,and the other from the T3 y2 to T3 y3. These two prominent transitions suggested significant transformation of the dynamic mechanism in the Helan basin.
Combined with conglomerate composition,strata thickness and sedimentary facies,heavymineral compositions were firstly used to study the provenances of the Middle-Late Triassic in the Helan Mountain. Results showed that the provenance of the Middle-Late Triassic sediments in the Helan Mountain were characterized by multiple and mixed sources,and were varied greatly. Sediments of the Middle Triassic Zhifang Formation were mainly from northwest and west. However,sediments of the Late Triassic Yanchang Formation changed. During deposition of the lower two members T3 y1 and T3 y2,sediments were mainly derived from the northwest,west and south. During deposition of the upper three members T3 y3 to T3 y5,eastern sources appeared,which were distributed in the Ruqigou to Xiangbangzigou. The western provenance was mainly in the sedimentary strata on the Alxa Block. Sediments of northwestern part were mainly from the Precambrian metamorphic rocks and Paleozoic magmatic rocks in the Paleoproterozoic Khondalite Belt,which was different from the southwestern part. Sediments in its eastern part were sourced from the sedimentary strata of Yinchuan graben and areas to its east. Provenance transformation of the Middle-Late Triassic strata in the Helan basin occurred twice: One from the Zhifang to Yanchang formations T3 y1,and the other from the T3 y2 to T3 y3. These two prominent transitions suggested significant transformation of the dynamic mechanism in the Helan basin.
引文
包创,陈岳龙,李大鹏.2013.内蒙古巴彦乌拉山古元古代斜长角闪岩LA-ICP-MS锆石U-Pb年龄和Hf同位素组成.地质通报,32(10):1513-1524.[Bao C,Chen Y L,Li D P.2013.LA-MC-ICP-MS zircons U-Pb dating and Hf isotopic compositions of the Paleoproterozoic amphibolite in Bayan Ul area,Inner Mongolia.Geological Bulletin of China,32(10):1513-1524]
白生明,吕昌国,郭永峰.2009.贺兰山中段古元古代赵池沟岩群的特征.宁夏工程技术,8(4):428-431.[Bai S M,LüC G,Guo YF.2009.The feature of the zhaochigou group complex in the middle of the Helan Mountains in Palaeoproterozoic.Ningxia Engineering Technology,8(4):428-431]
白云来,王新民,刘化清,李天顺.2006.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,80(6):792-813.[Bai Yl,Wang X M,Liu H Q,Li T S.2006.Determination of the border line of the western Ordos Basin and its geodynamics background.Acta Geologica Sinica,80(6):792-813]
陈刚.1999.中生代鄂尔多斯盆地陆源碎屑成分及其构造属性.沉积学报,17(3):409-413.[Chen G.1999.Terrigenous clastic composition and its tectonic feature in the Mesozoic of the Ordos Basin.Acta Sedimentologica Sinica,17(3):409-413]
陈志勇,杨帅师,孟二根,黄占起.2004.内蒙古阿拉善左旗巴音诺日公地区前寒武系的厘定.地质通报,23(4):345-351.[Chen ZY,Yang S S,Meng E G,Huang Z Q.2004.Revision of Precambrian stratigraphic units in the Bayan Nuru area,Alxa Zuoqi,Inner Mongolia.Geological Bulletin of China,23(4):345-351]
蔡佳,刘平华,刘福来,刘建辉,王舫,施建荣.2013.大青山-乌拉山变质杂岩带石拐地区富铝片麻岩成因矿物学与变质演化.岩石学报,29(2):437-461.[Cai J,Liu P H,Liu F L,Liu J H,Wang F,Shi J R.2013.Genetic mineralogy and metamorphic evolution of Al-rich gneisses in the Shiguai area,Daqingshan-Wulashan metamorphic complex belt.Acta Petrologica Sinica,29(2):437-461]
董春艳,刘敦一,李俊健,万渝生,周红英,李承东,杨岳衡,谢烈文.2007.华北克拉通西部孔兹岩带形成时代新证据:巴彦乌拉山-贺兰山地区锆石SHRIMP定年和Hf同位素组成.科学通报,52(16):1913-1922.[Dong C Y,Liu D Y,Li J J,Wan Y S,Zhou H Y,Li C D,Yang Y H,Xie L W.2007.New evidences about the formation age of the Khondalite belt in west North Craton:From the zircon SHRIMP dating and Hf isotopic composition in Bayanura and Helan Mountain region.Chinese Science Bulletin,52(16):1913-1922]
付星辉.2017.贺兰山上三叠统延长组沉积物源演化及构造意义.西北大学硕士论文,1-81.[Fu X H.2017.Analysis of Late Triassic Sedimentary Provenance and Its Tectonic Significance in the Helan Mountain.Doctoral Dissertation of Northwest University,1-81]
高山林.2001.鄂尔多斯盆地西缘中生代构造与地层分析及盆地演化研究.中国科学院地质与地球物理研究所博士论文,1-147.[Gao S L.2011.Mesozoic Tectonic and Stratigraphic Analysis and Basin Evolution in the Western Margin of Ordos Basin.Doctoral Dissertation of Institute of Geology and Geophysics,Chinese Academy of Sciences,1-147]
公王斌,胡健民,李振宏,董晓朋,刘洋,刘绍昌.2016.华北克拉通北缘裂谷渣尔泰群LA-ICP-MS碎屑锆石U-Pb测年及地质意义.岩石学报,32(7):2151-2165.[Gong W B,Hu J M,Li Z H,Dong X P,Liu Y,Liu S C.2016.Detrital zircon U-Pb dating of Zhaertai Group in the north margin rift zone of North China Craton and its implications.Acta Petrologica Sinica,32(7):2151-2165]
何自新.2003.鄂尔多斯盆地演化与油气.北京:石油工业出版社,1-390.[He Z X.2003.Evolution of Ordos Basin and Oil and Gas.Beijing:Petroleum Industry Press,1-390]
侯旭波,尹克敏,林中凯,韩秀艳,陈伟.2014.银川盆地构造反转及其演化与叠合关系分析.高校地质学报,20(2):277-285.[Hou X B,Yin K M,Lin Z K,Han X Y,Chen W.2014.The study of tectonic inversion,evolution,and superposition of Yinchuan Basin.Geological Journal of China Universities,20(2):277-285].
胡能高,杨家喜,王志博.1994.贺兰山变质杂岩的组成及演化.西安:西安地图出版社,1-121.[Hu N G,Yang J X,Wang Z B.1994.Composition and Evolution of Metamorphic Complex in Helan Mountions.Xi'an:Xi'an Map Press,1-121]
霍福臣,曹景轩,董燕生,顾其昌,阎志强.1987.贺兰山-阿拉善地区下、中前寒武系的划分对比及其变质、成矿作用特征.长春地质学院学报,17(1):35-46.[Huo F C,Cao J X,Dong Y S,Gu QC,Yan Z Q.1987.The division,correlation,metamorphism and mineralization features of the Lower and Middle Precambrian in the Helanshan Mountain-Alashan region,China.Journal of Changchun College of Geology,17(1):35-46]
贾承造,何登发,雷振宇.2000.前陆冲断带油气勘探.北京:石油工业出版社,1-351.[Jia C Z,He D F,Lei Z Y.2000.Oil and Gas Exploration in Foreland Thrust Belt.Beijing:Petroleum Industry Press,1-351]
柯保嘉,陈昌明,陈志明,汪寿松,陈景山,惠斌耀,姜好仁.1992.试论贺兰山地区延长群与鄂尔多斯盆地的关系.地质科学,27(2):124-130.[Ke B J,Chen C M,Chen Z M,Wang S S,Chen J S,Hui B Y,Jiang H R.1992.A discussion on the relationship between Upper Triassic sediments in Helanshan and Ordos.Scientia Geologica Sinica,27(2):124-130]
李俊健.2006.内蒙古阿拉善地块区域成矿系统.中国地质大学(北京)博士学位论文,1-175.[Li J J.2006.Regional metallogenic system of Alashan Block in Inner Monolia Autonomous Region.Doctoral Dissertation of China University of Geoscience(Beijing),1-175]
李黎明,曾佐勋,陆彦俊,魏运许,向世民,潘黎黎.2014.孔兹岩系-贺兰山中段赵池沟岩组碎屑锆石LA-ICP-MS锆石U-Pb年代学、Hf同位素组成及其地质意义.科学通报,59(7):593-604.[Li L M,Zeng Z X,Lu Y J,Wei Y X,Xiang S M,Pan L L.2014.LA-ICP-MS U-Pb geochronology of detrital zircons from the Zhaochigou Formation-complex in the Helan Mountain and its tectonic significance.Chinese Science Bulletin,59(7):593-604]
李蒙.2015.贺兰山地区晚三叠世延长期物源属性及其古构造意义.西北大学硕士学位论文,1-72.[Li M.2015.Long Term Provenance Properties of the Late Triassic Extension in the Helan Mountain Area and Its Tectonic Significance.Doctoral Dissertation of Northwest University,1-72]
李元昊.2008.鄂尔多斯盆地西部中区延长组下部石油成藏机理及主控因素.西北大学博士学位论文,1-152.[Li Y H.2008.The Oil Reservoir Forming Mechanisms and Its Main Controlling Factors of the Lower Yanchang Formation in the Middle of the West Ordos Basin.Doctoral Dissertation of Northwest University,1-152]
刘池洋,赵红格,桂小军,岳乐平,赵俊峰,王建强.2006.鄂尔多斯盆地演化-改造的时空坐标及其成藏(矿)响应.地质学报,80(5):617-638.[Liu C Y,Zhao H G,Gui X J,Yue L P,Zhao JF,Wang J Q.2006.Space-time coordinate of the evolution and reformation and mineralization response in Ordos Basin.Acta Geologica Sinica,80(5):617-638]
刘化清,李相博,陈启林,完颜容,郭彦如,廖建波.2013.鄂尔多斯盆地延长组若干石油地质问题分析.北京:科学出版社,1-169.[Liu H Q,Li X B,Chen Q L,Wanyan R,Guo Y R,Liao J B.2013.Analysis of Some Petroleum Geological Problems of Yanchang Formation in Ordos Basin.Beijing:Science Press,1-169]
刘建辉,张培震,郑德文,万景林.2010.贺兰山晚新生代隆升的剥露特征及其隆升模式.中国科学:地球科学,40(1):50-60.[Liu J H,Zhang P Z,Zheng D W,Wan J L.2010.Helan mountain late Cenozoic uplift and exhumation and uplift mode characteristics.Science China:Earth Science,40(1):50-60]
刘少峰,柯爱蓉,吴丽云,黄思骥.1997.鄂尔多斯西南缘前陆盆地沉积物物源分析及其构造意义.沉积学报,15(1):156-160.[Liu S F,Ke A R,Wu L Y,Huang S J.1997.Sediment provenance analysis and its tectonic significance in the foreland basin of the Ordos southwestern margin.Acta Sedimentologica Sinica,15(1):156-160]
卢良兆,徐学纯,刘福来.1996.中国北方早前寒武纪孔兹岩系.长春:长春出版社,1-176.[Lu L Z,Xu X C,Liu F L.1996.China in Early Precambrian Khondalite Series.Changchun:Changchun Press,1-176]
宁夏回族自治区地质矿产局.1990.宁夏回族自治区区域地质志.北京:地质出版社,260-339.[Ningxia Hui Autonomous Region Geological and Mineral Bureau.1990.Regional Geology of Ningxia Hui Autonomous Region.Beijing:Geological Publishing House,260-339]
彭润民,翟裕生,韩雪峰,王志刚,王建平,刘家军.2007.内蒙古狼山-渣尔泰山中元古代被动陆缘裂陷槽裂解过程中的火山活动及其示踪意义.岩石学报,23(5):1007-1017.[Peng R M,Zhai Y S,Han X F,Wang Z G,Wang J P,Liu J J.2007.Synsedimentry volcanic activities in the cracking process of the Mesoproterozoic aulacogen of passive continental margin in Langshan-Zhaertai area,Inner Mongolia,and its indicating significance.Acta Petrologica Sinica,23(5):1007-1017]
彭润民,翟裕生,王建平,陈喜峰,刘强,吕军阳,石永兴,王刚,李慎斌,王立功,马玉涛,张鹏.2010.内蒙狼山新元古代酸性火山岩的发现及其地质意义.科学通报,55(26):2611-2620.[Peng R M,Zhai Y S,Wang J P,Chen X F,Liu Q,LüJ Y,Shi Y X,Wang G,Li S B,Wang L G,Ma Y T,Zhang P.2010.Discovery of Neoproterozoic acid volcanic rock in the south-western section of Langshan,Inner Mongolia,and its geological significance.Chinese Science Bulletin,55(26):2611-2620]
彭润民,翟裕生,王建平,刘强.2015.华北地台北缘西段构造演化与狼山新元古代裂解-成矿作用.矿物学报,35(S1):537-538.[Peng R M,Zhai Y S,Wang J P,Liu Q.2015.Study on the northern part of the North China platform tectonic evolution and the Neoproterozoic lycocene-dissolved mineralization in Langshan.Acta Mineralogica Sinica,35(S1):537-538]
汤锡元,冯乔,李道燧.1990.内蒙古西部巴彦浩特盆地的构造特征及其演化.石油与天然气地质,11(2):127-135.[Tang X Y,Feng Q,Li D S.1990.Tectonic characteristics and evolution of the western Inner Mongolia Bayan Hot Basin.Oil and Gas Geology,11(2):127-135]
汤锡元,郭忠铭,陈荷立.1992.陕甘宁盆地西缘逆冲推覆构造及油气勘探.西安:西北大学出版社,1-392.[Tang X Y,Guo Z M,Chen H L.1992.The Western Ordos Basin Thrust Nappe Structure and Oil and Gas Exploration.Xi'an:Northwestern University Press,1-392]
魏红红,李文厚,邵磊,韩永林,杨阳,冀晓琳.2001.汝箕沟盆地上三叠统延长组沉积环境.西北大学学报,31(2):171-174.[Wei H H,Li W H,Shao L,Han Y L,Yang Y,Ji X L.2001.Sedimentary environment of Yanchang Formation of the Upper Triassic in Ruqigou Basin.Journal of Northwest University,31(2):171-174]
苏春乾,杨兴科,刘继庆,张忠义.2004.从贺兰山区的三叠-侏罗系论国内前陆盆地的研究.岩石矿物学杂志,23(4):318-326.[Su C Q,Yang X K,Liu J Q,Zhang Z Y.2004.A study of foreland basins in the light of Triassic-Jurassic strata of the Helan Mountain.Acta Petrologca et Mineralogica,23(4):318-326]
孙国凡,刘景平.1983.贺兰拗拉槽与前渊盆地及其演化.石油与天然气地质,4(3):242-245.[Sun G F,Liu J P.1983.Helan aulacogen and front basin and their evolution.Oil and Gas Geology,4(3):236-245]
沈存利,张梅,杨帅师.2009.华北陆块北缘西段狼山-渣尔泰山裂陷槽西延的地质依据及其意义.地质与勘探,45(6):661-668.[Shen C L,Zhang M,Yang S S.2009.The geological evidences and significance of westward extension of Langshan-Zhaertaishan rift system,northern margin of North China Terrane.Geology and Exploration,45(6):661-668]
王成,孟方,毛自力.2012.贺兰山黄旗口花岗岩锆石SHRIMP U-Pb定年和岩石地球化学特征.宁夏工程技术,11(3):206-213.[Wang C,Meng F,Mai Z L.2012.Zircon SHRIMP U-Pb dating technique for Huangqikou granite in Helanshan area and its lithogeochemical characteristics.Ningxia Engineering Technology,11(3):206-213]
王锋.2006.贺兰山中段中生代构造环境分析.西北大学博士论文,1-103.[Wang F.2006.Analysis of Mesozoic Tectonic Environment in the Middle Part of Helan Mountain.Doctoral Dissertation of Northwest University,1-103]
王锋,刘池洋,赵红格,杨兴科,翁望飞.2006a.贺兰山西麓中生代构造反转及意义.石油实验地质,28(3):206-209.[Wang F,Liu C Y,Zhao H G,Yang X K,Weng W F.2006a.Tectonic reverse of Mesozoic at the western foot of Helan Mountain and its meaning.Petroleum Geology and Experiment,28(3):206-209]
王锋,刘池洋,赵红格,杨兴科,苏春乾.2006b.贺兰山盆地与鄂尔多斯盆地的关系.石油学报,27(4):15-17.[Wang F,Liu C Y,Zhao H G,Yang X K,Su C Q.2006b.Relationship between Helanshan Basin and Ordos Basin.Acta Petrolei Sinica,27(4):15-17]
万渝生,耿元生,刘福来,沈其韩,刘敦一,宋彪.2000.华北克拉通及邻区孔兹岩系的时代及对太古宙基底组成的制约.前寒武纪研究进展,23(4):221-237.[Wan Y S,Geng Y S,Liu F L,Shen QH,Liu D Y,Song B.2000.Age and composition of the Khondalite series of the North China Craton and its adjacent area.Progress in Precambrian Research,23(4):221-237]
吴泰然,何国琦.1993.内蒙古阿拉善地块北缘的构造单元划分及各单元的基本特征.地质学报,67(2):97-108.[Wu T R,He GQ.1993.Tectonic units and their fundamental characteristics on the northern margin of the Alxa Block.Acta Geologica Sinica,67(2):97-108]
杨福新.1998.内蒙狼山地区糜棱岩岩石特征及构造意义.西北地质,19(1):1-8.[Yang F X.1998.The characteristics and tectonic significance of rocks in Langshan area of Inner Mongolia.Northwest Geology,19(1):1-8]
杨华,付金华,欧阳征健,孙六一,马占荣.2010.鄂尔多斯盆地西缘汝箕沟大岭-鼓鼓台玄武岩锆石U-Pb定年及其构造意义.地球学报,31(2):229-236.[Yang H,Fu J H,Ouyang Z J,Sun LY,Ma Z R.2010.U-Pb zircon dating of the Daling-Gugutai basalt in Rujigou on the western margin of Ordos Basin.Acta Geoscientica Sinica,31(2):229-236]
杨华,付金华,欧阳征健,孙六一.2011.鄂尔多斯盆地西缘晚三叠世构造-沉积环境分析.沉积学报,29(3):437-439.[Yang H,Fu J H,Ouyang Z J,Sun L Y.2011.Analysis of tectonic-sedimentary setting in Middle and Upper Triassic in the west margin of the Ordos Basin.Acta Sedimentologica Sinica,29(3):437-439]
杨俊杰,李克勤.1992.中国石油地质志(卷120)·长庆油田.北京:石油工业出版社,1-490.[Yang J J,Li K Q.1992.Petroleum Geology of China:Changqing Oilfield.Beijing:Petroleum Industry Press,1-490]
叶连俊.1983.华北地台沉积建造.北京:科学出版社,110-128.[Ye L J.1983.Sedimentary Buildings in North China Block.Beijing:Science Press,110-128]
张岳桥,施炜,廖昌珍,胡博.2006.鄂尔多斯盆地周边断裂运动学分析与晚中生代构造应力体制转换.地质学报,80(5):639-647.[Zhang Y Q,Shi W,Liao C Z,Hu B.2006.Fault kinematic analysis and change in Late Mesozoic tectonic stress regimes in the peripheral zones of the Ordos Basin,North China.Acta Geologica Sinica,80(5):639-647]
张进,马宗晋,任文军.2004.再论贺兰山地区新生代之前拉张活动的性质.石油学报,25(6):8-11.[Zhang J,Ma Z J,Ren W J.2004.Re-discussion on natures of extension in Helanshan region before Cenozoic Era.Acta Petrolei Sinica,25(6):8-11]
张进,李锦铁,马宗晋,任文军.2009.贺兰山三叠纪盆地构造属性再分析.地质学报,83(9):1233-1246.[Zhang J,Li J T,Ma Z J,Ren W J.2009.The tectonic setting of the Triassic basin in the Helanshan Mt.Acta Geologica Sinica,83(9):1233-1246]
张义楷.2007.鄂尔多斯西缘中新生代构造体制转换与油气聚集.西北大学博士学位论文,1-195.[Zhang Y K.2007.Transition of the Mesozoic-Cenozoic Tectonic Regimes and Hydrocarbon Accumulation in Western Ordos Region.Doctoral Dissertation of Northwest University,1-195]
赵红格.2003.鄂尔多斯盆地西部构造特征及演化.西北大学博士学位论文,1-143.[Zhao H G.2003.Structural Characteristics and Evolution in western Ordos Basin.Doctoral Dissertation of Northwest University,1-143]
赵红格,刘池洋,王锋,王建强,李琼,姚亚明.2007.贺兰山隆升时限及其演化.中国科学D辑:地球科学,37(增刊Ⅰ):185-192.[Zhao H G,Liu C Y,Wang F,Wang J Q,Li Q,Yao Y M.2007.Upilft and evolution of Helan Mountain.Sciencein China:Series D,37(SupplementⅠ):185-192]
赵红格,刘池洋,王海然,乔建新,王建强,冯晓博.2012.贺兰山北段晚三叠世沉积物源分析.沉积学报,30(4):654-660.[Zhao HG,Liu C Y,Wang H R,Qiao J X,Wang J Q,Feng X B.2012.Analysis of Late Triassic sedimentary provenance in the north of Helan Mountain.Acta Sedimentologica Sinica,30(4):654-660]
赵文智,王新民,郭彦如,刘华清,白云来.2006.鄂尔多斯盆地西部晚三叠世原型盆地恢复及其改造演化.石油勘探与开发,33(1):6-13.[Zhao W Z,Wang X M,Guo Y R,Liu H Q,Bai YL.2006.Restoration and tectonic reworking of the Late Triassic basin in western Ordos Basin.Petroleum Exploration and Development,33(1):6-13]
钟长汀,邓晋福,万渝生,涂伟萍.2014.内蒙古大青山地区古元古代花岗岩:地球化学、锆石SHRIMP定年及其地质意义.岩石学报,30(11):3172-3188.[Zhong C T,Deng J F,Wan Y S,Tu WQ.2014.Paleoproterozoic granitoids in the Daqingshan Mountain area,Inner Mongolia:Geochemistry,SHRIMP zircon dating and geological significance.Acta Petrologica Sinica,30(11):3172-3188]
周喜文,耿元生.2009.贺兰山孔兹岩系的变质时代及其对华北克拉通西部陆块演化的制约.岩石学报,25(8):1843-1852.[Zhou X W,Geng Y S.2009.Metamorphic age of the Khondalite series in the Helanshan region:Evolution of the western block in the North China Craton.Acta Petrologica Sinica,25(8):1843-1852]
Cawood P A.1990.Provenance mixing in an intraoceanic subduction zone:Tonga Trench-Louisville Ridge collision zone,southwest Pacific.Sedimentary Geology,67(1-2):35-53.
Darby B J,Ritts B D.2002.Mesozoic contractional deformation in the middle of the Asian tectonic collage:The intraplate Western Ordos fold-thrust belt,China.Earth and Planetary Science Letters,205(1):13-24.
Darby B J.2003.Mesozoic intraplate deformation in the east Asian tectonic collage:The enigmatic Northwest Ordos Region,China.Doctoral Dissertation of University of Southern California,1-173.
Henry D J.1985.Tourmaline as a petrogenetic indicator mineral:An example from the staurolite-grade metapelites of NW Maine.American Mineralogist,70(1):1-15.
Hubert J F.1962.A zircon-tourmaline-rutile maturity index and the interdependence of the composition of heavy minerals assemblages with the gross composition and texture of sandstones.Journal of Sedimentary Research,32(3):440-450.
Liu S F.1998.The coupling mechanism of basin and orogen in the western Ordos Basin and adjacent regions of China.Journal of Asian Earth Sciences,16(4):369-383.
Mange-Rajetzky M A.1981.Detrital blue sodic amphibole in recent sediments,southern coast,Turkey.Journal of the Geological Society of London,138(1):83-92.
Morton A C,Whitham A G,Fanning C M.2005.Provenance of Late Cretaceous to Paleocene submarine fan sandstones in the Norwegian Sea:Integration of heavy mineral,mineral chemical and zircon age data.Sedimentary Geology,182(1-4):3-28.
Hu J M,Gong W B,Wu S J,Liu Y,Liu S C.2014.LA-ICP-MS zircon U-Pb dating of the Langshan Group in the northeast margin of the Alxa block,with tectonic implications.Precambrian Research,255:756-770.
Ritts B D,Hanson A D,Darby B J,Nanson L,Berry A.2004.Sedimentary record of Triassic intraplate extension in North China:Evidence from the nonmarine NW Ordos Basin,Helan Shan and Zhuozi Shan.Tectonophysics,386(3-4):177-202.
Ritts B D,Dustin K,Darby B J,Liu S F.2006.Ordos Basin gas reservoir outcrop analogs:Permian braided fluvial sandstone of the Zhuozi Shan and Helan Shan,China.International Geology Review,48(7):573-584.
Sabeen H M,Ramanujam N,Morton A C.2002.The provenance of garnet:Constraints provided by studies of coastal sediments from southern India.Sedimentary Geology,152(3):279-287.
Takeuchi M.1994.Changes in garnet chemistry show a progressive denudation of the source areas for Permian-Jurassic sandstones,Southern Kitakami Terrane,Japan.Sedimentary Geology,93(1-2):85-105.
(1)宁夏地质局区域地质调查队.1982a.阿拉善左旗幅1︰200000区域地质调查报告.1-139.
(2)宁夏地质局区域地质调查队.1982b.石嘴山市幅1︰200000区域地质调查报告.1-162.
(1)宁夏地质局区域地质调查队.1982b.石嘴山市幅1︰200000区域地质调查报告.1-162.
(1)宁夏地质局区域地质调查队.1982a.阿拉善左旗幅1︰200000区域地质调查报告.1-139.
(2)宁夏地质局区域地质调查队.1982b.石嘴山市幅1︰200000区域地质调查报告.1-162.
白生明,吕昌国,郭永峰.2009.贺兰山中段古元古代赵池沟岩群的特征.宁夏工程技术,8(4):428-431.[Bai S M,LüC G,Guo YF.2009.The feature of the zhaochigou group complex in the middle of the Helan Mountains in Palaeoproterozoic.Ningxia Engineering Technology,8(4):428-431]
白云来,王新民,刘化清,李天顺.2006.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,80(6):792-813.[Bai Yl,Wang X M,Liu H Q,Li T S.2006.Determination of the border line of the western Ordos Basin and its geodynamics background.Acta Geologica Sinica,80(6):792-813]
陈刚.1999.中生代鄂尔多斯盆地陆源碎屑成分及其构造属性.沉积学报,17(3):409-413.[Chen G.1999.Terrigenous clastic composition and its tectonic feature in the Mesozoic of the Ordos Basin.Acta Sedimentologica Sinica,17(3):409-413]
陈志勇,杨帅师,孟二根,黄占起.2004.内蒙古阿拉善左旗巴音诺日公地区前寒武系的厘定.地质通报,23(4):345-351.[Chen ZY,Yang S S,Meng E G,Huang Z Q.2004.Revision of Precambrian stratigraphic units in the Bayan Nuru area,Alxa Zuoqi,Inner Mongolia.Geological Bulletin of China,23(4):345-351]
蔡佳,刘平华,刘福来,刘建辉,王舫,施建荣.2013.大青山-乌拉山变质杂岩带石拐地区富铝片麻岩成因矿物学与变质演化.岩石学报,29(2):437-461.[Cai J,Liu P H,Liu F L,Liu J H,Wang F,Shi J R.2013.Genetic mineralogy and metamorphic evolution of Al-rich gneisses in the Shiguai area,Daqingshan-Wulashan metamorphic complex belt.Acta Petrologica Sinica,29(2):437-461]
董春艳,刘敦一,李俊健,万渝生,周红英,李承东,杨岳衡,谢烈文.2007.华北克拉通西部孔兹岩带形成时代新证据:巴彦乌拉山-贺兰山地区锆石SHRIMP定年和Hf同位素组成.科学通报,52(16):1913-1922.[Dong C Y,Liu D Y,Li J J,Wan Y S,Zhou H Y,Li C D,Yang Y H,Xie L W.2007.New evidences about the formation age of the Khondalite belt in west North Craton:From the zircon SHRIMP dating and Hf isotopic composition in Bayanura and Helan Mountain region.Chinese Science Bulletin,52(16):1913-1922]
付星辉.2017.贺兰山上三叠统延长组沉积物源演化及构造意义.西北大学硕士论文,1-81.[Fu X H.2017.Analysis of Late Triassic Sedimentary Provenance and Its Tectonic Significance in the Helan Mountain.Doctoral Dissertation of Northwest University,1-81]
高山林.2001.鄂尔多斯盆地西缘中生代构造与地层分析及盆地演化研究.中国科学院地质与地球物理研究所博士论文,1-147.[Gao S L.2011.Mesozoic Tectonic and Stratigraphic Analysis and Basin Evolution in the Western Margin of Ordos Basin.Doctoral Dissertation of Institute of Geology and Geophysics,Chinese Academy of Sciences,1-147]
公王斌,胡健民,李振宏,董晓朋,刘洋,刘绍昌.2016.华北克拉通北缘裂谷渣尔泰群LA-ICP-MS碎屑锆石U-Pb测年及地质意义.岩石学报,32(7):2151-2165.[Gong W B,Hu J M,Li Z H,Dong X P,Liu Y,Liu S C.2016.Detrital zircon U-Pb dating of Zhaertai Group in the north margin rift zone of North China Craton and its implications.Acta Petrologica Sinica,32(7):2151-2165]
何自新.2003.鄂尔多斯盆地演化与油气.北京:石油工业出版社,1-390.[He Z X.2003.Evolution of Ordos Basin and Oil and Gas.Beijing:Petroleum Industry Press,1-390]
侯旭波,尹克敏,林中凯,韩秀艳,陈伟.2014.银川盆地构造反转及其演化与叠合关系分析.高校地质学报,20(2):277-285.[Hou X B,Yin K M,Lin Z K,Han X Y,Chen W.2014.The study of tectonic inversion,evolution,and superposition of Yinchuan Basin.Geological Journal of China Universities,20(2):277-285].
胡能高,杨家喜,王志博.1994.贺兰山变质杂岩的组成及演化.西安:西安地图出版社,1-121.[Hu N G,Yang J X,Wang Z B.1994.Composition and Evolution of Metamorphic Complex in Helan Mountions.Xi'an:Xi'an Map Press,1-121]
霍福臣,曹景轩,董燕生,顾其昌,阎志强.1987.贺兰山-阿拉善地区下、中前寒武系的划分对比及其变质、成矿作用特征.长春地质学院学报,17(1):35-46.[Huo F C,Cao J X,Dong Y S,Gu QC,Yan Z Q.1987.The division,correlation,metamorphism and mineralization features of the Lower and Middle Precambrian in the Helanshan Mountain-Alashan region,China.Journal of Changchun College of Geology,17(1):35-46]
贾承造,何登发,雷振宇.2000.前陆冲断带油气勘探.北京:石油工业出版社,1-351.[Jia C Z,He D F,Lei Z Y.2000.Oil and Gas Exploration in Foreland Thrust Belt.Beijing:Petroleum Industry Press,1-351]
柯保嘉,陈昌明,陈志明,汪寿松,陈景山,惠斌耀,姜好仁.1992.试论贺兰山地区延长群与鄂尔多斯盆地的关系.地质科学,27(2):124-130.[Ke B J,Chen C M,Chen Z M,Wang S S,Chen J S,Hui B Y,Jiang H R.1992.A discussion on the relationship between Upper Triassic sediments in Helanshan and Ordos.Scientia Geologica Sinica,27(2):124-130]
李俊健.2006.内蒙古阿拉善地块区域成矿系统.中国地质大学(北京)博士学位论文,1-175.[Li J J.2006.Regional metallogenic system of Alashan Block in Inner Monolia Autonomous Region.Doctoral Dissertation of China University of Geoscience(Beijing),1-175]
李黎明,曾佐勋,陆彦俊,魏运许,向世民,潘黎黎.2014.孔兹岩系-贺兰山中段赵池沟岩组碎屑锆石LA-ICP-MS锆石U-Pb年代学、Hf同位素组成及其地质意义.科学通报,59(7):593-604.[Li L M,Zeng Z X,Lu Y J,Wei Y X,Xiang S M,Pan L L.2014.LA-ICP-MS U-Pb geochronology of detrital zircons from the Zhaochigou Formation-complex in the Helan Mountain and its tectonic significance.Chinese Science Bulletin,59(7):593-604]
李蒙.2015.贺兰山地区晚三叠世延长期物源属性及其古构造意义.西北大学硕士学位论文,1-72.[Li M.2015.Long Term Provenance Properties of the Late Triassic Extension in the Helan Mountain Area and Its Tectonic Significance.Doctoral Dissertation of Northwest University,1-72]
李元昊.2008.鄂尔多斯盆地西部中区延长组下部石油成藏机理及主控因素.西北大学博士学位论文,1-152.[Li Y H.2008.The Oil Reservoir Forming Mechanisms and Its Main Controlling Factors of the Lower Yanchang Formation in the Middle of the West Ordos Basin.Doctoral Dissertation of Northwest University,1-152]
刘池洋,赵红格,桂小军,岳乐平,赵俊峰,王建强.2006.鄂尔多斯盆地演化-改造的时空坐标及其成藏(矿)响应.地质学报,80(5):617-638.[Liu C Y,Zhao H G,Gui X J,Yue L P,Zhao JF,Wang J Q.2006.Space-time coordinate of the evolution and reformation and mineralization response in Ordos Basin.Acta Geologica Sinica,80(5):617-638]
刘化清,李相博,陈启林,完颜容,郭彦如,廖建波.2013.鄂尔多斯盆地延长组若干石油地质问题分析.北京:科学出版社,1-169.[Liu H Q,Li X B,Chen Q L,Wanyan R,Guo Y R,Liao J B.2013.Analysis of Some Petroleum Geological Problems of Yanchang Formation in Ordos Basin.Beijing:Science Press,1-169]
刘建辉,张培震,郑德文,万景林.2010.贺兰山晚新生代隆升的剥露特征及其隆升模式.中国科学:地球科学,40(1):50-60.[Liu J H,Zhang P Z,Zheng D W,Wan J L.2010.Helan mountain late Cenozoic uplift and exhumation and uplift mode characteristics.Science China:Earth Science,40(1):50-60]
刘少峰,柯爱蓉,吴丽云,黄思骥.1997.鄂尔多斯西南缘前陆盆地沉积物物源分析及其构造意义.沉积学报,15(1):156-160.[Liu S F,Ke A R,Wu L Y,Huang S J.1997.Sediment provenance analysis and its tectonic significance in the foreland basin of the Ordos southwestern margin.Acta Sedimentologica Sinica,15(1):156-160]
卢良兆,徐学纯,刘福来.1996.中国北方早前寒武纪孔兹岩系.长春:长春出版社,1-176.[Lu L Z,Xu X C,Liu F L.1996.China in Early Precambrian Khondalite Series.Changchun:Changchun Press,1-176]
宁夏回族自治区地质矿产局.1990.宁夏回族自治区区域地质志.北京:地质出版社,260-339.[Ningxia Hui Autonomous Region Geological and Mineral Bureau.1990.Regional Geology of Ningxia Hui Autonomous Region.Beijing:Geological Publishing House,260-339]
彭润民,翟裕生,韩雪峰,王志刚,王建平,刘家军.2007.内蒙古狼山-渣尔泰山中元古代被动陆缘裂陷槽裂解过程中的火山活动及其示踪意义.岩石学报,23(5):1007-1017.[Peng R M,Zhai Y S,Han X F,Wang Z G,Wang J P,Liu J J.2007.Synsedimentry volcanic activities in the cracking process of the Mesoproterozoic aulacogen of passive continental margin in Langshan-Zhaertai area,Inner Mongolia,and its indicating significance.Acta Petrologica Sinica,23(5):1007-1017]
彭润民,翟裕生,王建平,陈喜峰,刘强,吕军阳,石永兴,王刚,李慎斌,王立功,马玉涛,张鹏.2010.内蒙狼山新元古代酸性火山岩的发现及其地质意义.科学通报,55(26):2611-2620.[Peng R M,Zhai Y S,Wang J P,Chen X F,Liu Q,LüJ Y,Shi Y X,Wang G,Li S B,Wang L G,Ma Y T,Zhang P.2010.Discovery of Neoproterozoic acid volcanic rock in the south-western section of Langshan,Inner Mongolia,and its geological significance.Chinese Science Bulletin,55(26):2611-2620]
彭润民,翟裕生,王建平,刘强.2015.华北地台北缘西段构造演化与狼山新元古代裂解-成矿作用.矿物学报,35(S1):537-538.[Peng R M,Zhai Y S,Wang J P,Liu Q.2015.Study on the northern part of the North China platform tectonic evolution and the Neoproterozoic lycocene-dissolved mineralization in Langshan.Acta Mineralogica Sinica,35(S1):537-538]
汤锡元,冯乔,李道燧.1990.内蒙古西部巴彦浩特盆地的构造特征及其演化.石油与天然气地质,11(2):127-135.[Tang X Y,Feng Q,Li D S.1990.Tectonic characteristics and evolution of the western Inner Mongolia Bayan Hot Basin.Oil and Gas Geology,11(2):127-135]
汤锡元,郭忠铭,陈荷立.1992.陕甘宁盆地西缘逆冲推覆构造及油气勘探.西安:西北大学出版社,1-392.[Tang X Y,Guo Z M,Chen H L.1992.The Western Ordos Basin Thrust Nappe Structure and Oil and Gas Exploration.Xi'an:Northwestern University Press,1-392]
魏红红,李文厚,邵磊,韩永林,杨阳,冀晓琳.2001.汝箕沟盆地上三叠统延长组沉积环境.西北大学学报,31(2):171-174.[Wei H H,Li W H,Shao L,Han Y L,Yang Y,Ji X L.2001.Sedimentary environment of Yanchang Formation of the Upper Triassic in Ruqigou Basin.Journal of Northwest University,31(2):171-174]
苏春乾,杨兴科,刘继庆,张忠义.2004.从贺兰山区的三叠-侏罗系论国内前陆盆地的研究.岩石矿物学杂志,23(4):318-326.[Su C Q,Yang X K,Liu J Q,Zhang Z Y.2004.A study of foreland basins in the light of Triassic-Jurassic strata of the Helan Mountain.Acta Petrologca et Mineralogica,23(4):318-326]
孙国凡,刘景平.1983.贺兰拗拉槽与前渊盆地及其演化.石油与天然气地质,4(3):242-245.[Sun G F,Liu J P.1983.Helan aulacogen and front basin and their evolution.Oil and Gas Geology,4(3):236-245]
沈存利,张梅,杨帅师.2009.华北陆块北缘西段狼山-渣尔泰山裂陷槽西延的地质依据及其意义.地质与勘探,45(6):661-668.[Shen C L,Zhang M,Yang S S.2009.The geological evidences and significance of westward extension of Langshan-Zhaertaishan rift system,northern margin of North China Terrane.Geology and Exploration,45(6):661-668]
王成,孟方,毛自力.2012.贺兰山黄旗口花岗岩锆石SHRIMP U-Pb定年和岩石地球化学特征.宁夏工程技术,11(3):206-213.[Wang C,Meng F,Mai Z L.2012.Zircon SHRIMP U-Pb dating technique for Huangqikou granite in Helanshan area and its lithogeochemical characteristics.Ningxia Engineering Technology,11(3):206-213]
王锋.2006.贺兰山中段中生代构造环境分析.西北大学博士论文,1-103.[Wang F.2006.Analysis of Mesozoic Tectonic Environment in the Middle Part of Helan Mountain.Doctoral Dissertation of Northwest University,1-103]
王锋,刘池洋,赵红格,杨兴科,翁望飞.2006a.贺兰山西麓中生代构造反转及意义.石油实验地质,28(3):206-209.[Wang F,Liu C Y,Zhao H G,Yang X K,Weng W F.2006a.Tectonic reverse of Mesozoic at the western foot of Helan Mountain and its meaning.Petroleum Geology and Experiment,28(3):206-209]
王锋,刘池洋,赵红格,杨兴科,苏春乾.2006b.贺兰山盆地与鄂尔多斯盆地的关系.石油学报,27(4):15-17.[Wang F,Liu C Y,Zhao H G,Yang X K,Su C Q.2006b.Relationship between Helanshan Basin and Ordos Basin.Acta Petrolei Sinica,27(4):15-17]
万渝生,耿元生,刘福来,沈其韩,刘敦一,宋彪.2000.华北克拉通及邻区孔兹岩系的时代及对太古宙基底组成的制约.前寒武纪研究进展,23(4):221-237.[Wan Y S,Geng Y S,Liu F L,Shen QH,Liu D Y,Song B.2000.Age and composition of the Khondalite series of the North China Craton and its adjacent area.Progress in Precambrian Research,23(4):221-237]
吴泰然,何国琦.1993.内蒙古阿拉善地块北缘的构造单元划分及各单元的基本特征.地质学报,67(2):97-108.[Wu T R,He GQ.1993.Tectonic units and their fundamental characteristics on the northern margin of the Alxa Block.Acta Geologica Sinica,67(2):97-108]
杨福新.1998.内蒙狼山地区糜棱岩岩石特征及构造意义.西北地质,19(1):1-8.[Yang F X.1998.The characteristics and tectonic significance of rocks in Langshan area of Inner Mongolia.Northwest Geology,19(1):1-8]
杨华,付金华,欧阳征健,孙六一,马占荣.2010.鄂尔多斯盆地西缘汝箕沟大岭-鼓鼓台玄武岩锆石U-Pb定年及其构造意义.地球学报,31(2):229-236.[Yang H,Fu J H,Ouyang Z J,Sun LY,Ma Z R.2010.U-Pb zircon dating of the Daling-Gugutai basalt in Rujigou on the western margin of Ordos Basin.Acta Geoscientica Sinica,31(2):229-236]
杨华,付金华,欧阳征健,孙六一.2011.鄂尔多斯盆地西缘晚三叠世构造-沉积环境分析.沉积学报,29(3):437-439.[Yang H,Fu J H,Ouyang Z J,Sun L Y.2011.Analysis of tectonic-sedimentary setting in Middle and Upper Triassic in the west margin of the Ordos Basin.Acta Sedimentologica Sinica,29(3):437-439]
杨俊杰,李克勤.1992.中国石油地质志(卷120)·长庆油田.北京:石油工业出版社,1-490.[Yang J J,Li K Q.1992.Petroleum Geology of China:Changqing Oilfield.Beijing:Petroleum Industry Press,1-490]
叶连俊.1983.华北地台沉积建造.北京:科学出版社,110-128.[Ye L J.1983.Sedimentary Buildings in North China Block.Beijing:Science Press,110-128]
张岳桥,施炜,廖昌珍,胡博.2006.鄂尔多斯盆地周边断裂运动学分析与晚中生代构造应力体制转换.地质学报,80(5):639-647.[Zhang Y Q,Shi W,Liao C Z,Hu B.2006.Fault kinematic analysis and change in Late Mesozoic tectonic stress regimes in the peripheral zones of the Ordos Basin,North China.Acta Geologica Sinica,80(5):639-647]
张进,马宗晋,任文军.2004.再论贺兰山地区新生代之前拉张活动的性质.石油学报,25(6):8-11.[Zhang J,Ma Z J,Ren W J.2004.Re-discussion on natures of extension in Helanshan region before Cenozoic Era.Acta Petrolei Sinica,25(6):8-11]
张进,李锦铁,马宗晋,任文军.2009.贺兰山三叠纪盆地构造属性再分析.地质学报,83(9):1233-1246.[Zhang J,Li J T,Ma Z J,Ren W J.2009.The tectonic setting of the Triassic basin in the Helanshan Mt.Acta Geologica Sinica,83(9):1233-1246]
张义楷.2007.鄂尔多斯西缘中新生代构造体制转换与油气聚集.西北大学博士学位论文,1-195.[Zhang Y K.2007.Transition of the Mesozoic-Cenozoic Tectonic Regimes and Hydrocarbon Accumulation in Western Ordos Region.Doctoral Dissertation of Northwest University,1-195]
赵红格.2003.鄂尔多斯盆地西部构造特征及演化.西北大学博士学位论文,1-143.[Zhao H G.2003.Structural Characteristics and Evolution in western Ordos Basin.Doctoral Dissertation of Northwest University,1-143]
赵红格,刘池洋,王锋,王建强,李琼,姚亚明.2007.贺兰山隆升时限及其演化.中国科学D辑:地球科学,37(增刊Ⅰ):185-192.[Zhao H G,Liu C Y,Wang F,Wang J Q,Li Q,Yao Y M.2007.Upilft and evolution of Helan Mountain.Sciencein China:Series D,37(SupplementⅠ):185-192]
赵红格,刘池洋,王海然,乔建新,王建强,冯晓博.2012.贺兰山北段晚三叠世沉积物源分析.沉积学报,30(4):654-660.[Zhao HG,Liu C Y,Wang H R,Qiao J X,Wang J Q,Feng X B.2012.Analysis of Late Triassic sedimentary provenance in the north of Helan Mountain.Acta Sedimentologica Sinica,30(4):654-660]
赵文智,王新民,郭彦如,刘华清,白云来.2006.鄂尔多斯盆地西部晚三叠世原型盆地恢复及其改造演化.石油勘探与开发,33(1):6-13.[Zhao W Z,Wang X M,Guo Y R,Liu H Q,Bai YL.2006.Restoration and tectonic reworking of the Late Triassic basin in western Ordos Basin.Petroleum Exploration and Development,33(1):6-13]
钟长汀,邓晋福,万渝生,涂伟萍.2014.内蒙古大青山地区古元古代花岗岩:地球化学、锆石SHRIMP定年及其地质意义.岩石学报,30(11):3172-3188.[Zhong C T,Deng J F,Wan Y S,Tu WQ.2014.Paleoproterozoic granitoids in the Daqingshan Mountain area,Inner Mongolia:Geochemistry,SHRIMP zircon dating and geological significance.Acta Petrologica Sinica,30(11):3172-3188]
周喜文,耿元生.2009.贺兰山孔兹岩系的变质时代及其对华北克拉通西部陆块演化的制约.岩石学报,25(8):1843-1852.[Zhou X W,Geng Y S.2009.Metamorphic age of the Khondalite series in the Helanshan region:Evolution of the western block in the North China Craton.Acta Petrologica Sinica,25(8):1843-1852]
Cawood P A.1990.Provenance mixing in an intraoceanic subduction zone:Tonga Trench-Louisville Ridge collision zone,southwest Pacific.Sedimentary Geology,67(1-2):35-53.
Darby B J,Ritts B D.2002.Mesozoic contractional deformation in the middle of the Asian tectonic collage:The intraplate Western Ordos fold-thrust belt,China.Earth and Planetary Science Letters,205(1):13-24.
Darby B J.2003.Mesozoic intraplate deformation in the east Asian tectonic collage:The enigmatic Northwest Ordos Region,China.Doctoral Dissertation of University of Southern California,1-173.
Henry D J.1985.Tourmaline as a petrogenetic indicator mineral:An example from the staurolite-grade metapelites of NW Maine.American Mineralogist,70(1):1-15.
Hubert J F.1962.A zircon-tourmaline-rutile maturity index and the interdependence of the composition of heavy minerals assemblages with the gross composition and texture of sandstones.Journal of Sedimentary Research,32(3):440-450.
Liu S F.1998.The coupling mechanism of basin and orogen in the western Ordos Basin and adjacent regions of China.Journal of Asian Earth Sciences,16(4):369-383.
Mange-Rajetzky M A.1981.Detrital blue sodic amphibole in recent sediments,southern coast,Turkey.Journal of the Geological Society of London,138(1):83-92.
Morton A C,Whitham A G,Fanning C M.2005.Provenance of Late Cretaceous to Paleocene submarine fan sandstones in the Norwegian Sea:Integration of heavy mineral,mineral chemical and zircon age data.Sedimentary Geology,182(1-4):3-28.
Hu J M,Gong W B,Wu S J,Liu Y,Liu S C.2014.LA-ICP-MS zircon U-Pb dating of the Langshan Group in the northeast margin of the Alxa block,with tectonic implications.Precambrian Research,255:756-770.
Ritts B D,Hanson A D,Darby B J,Nanson L,Berry A.2004.Sedimentary record of Triassic intraplate extension in North China:Evidence from the nonmarine NW Ordos Basin,Helan Shan and Zhuozi Shan.Tectonophysics,386(3-4):177-202.
Ritts B D,Dustin K,Darby B J,Liu S F.2006.Ordos Basin gas reservoir outcrop analogs:Permian braided fluvial sandstone of the Zhuozi Shan and Helan Shan,China.International Geology Review,48(7):573-584.
Sabeen H M,Ramanujam N,Morton A C.2002.The provenance of garnet:Constraints provided by studies of coastal sediments from southern India.Sedimentary Geology,152(3):279-287.
Takeuchi M.1994.Changes in garnet chemistry show a progressive denudation of the source areas for Permian-Jurassic sandstones,Southern Kitakami Terrane,Japan.Sedimentary Geology,93(1-2):85-105.
(1)宁夏地质局区域地质调查队.1982a.阿拉善左旗幅1︰200000区域地质调查报告.1-139.
(2)宁夏地质局区域地质调查队.1982b.石嘴山市幅1︰200000区域地质调查报告.1-162.
(1)宁夏地质局区域地质调查队.1982b.石嘴山市幅1︰200000区域地质调查报告.1-162.
(1)宁夏地质局区域地质调查队.1982a.阿拉善左旗幅1︰200000区域地质调查报告.1-139.
(2)宁夏地质局区域地质调查队.1982b.石嘴山市幅1︰200000区域地质调查报告.1-162.