吉林汪清早二叠世和盛植物群
|
摘要
石炭—二叠纪全球发育四大植物群：华夏植物群、欧美植物群、安加拉植物群和冈瓦纳植物群。中国东北地区南、北分属于华夏植物地理大区和安加拉植物地理大区，两大区系的界线位置位于西拉木伦河一线。然而，两大植物地理区系界线在东北东部的延伸位置仍不明晰。同时，吉林延边地区的地层学研究极其混乱，甚至有人认为延边石炭—二叠系属于蛇绿杂岩、浊积—混杂岩系。上述问题的存在严重影响了索伦—西拉木伦河缝合带在延边地区延伸位置的确定。
为了确定东北东部二叠纪华夏植物群与安加拉植物群区系界线位置、查明延边地区地层发育序列、分析索伦—西拉木伦河缝合带在延边地区的延伸位置，本文首次对中国吉林省汪清县大兴沟镇和盛植物群进行了系统的古植物学研究，对植物化石产地进行了深入的地层学探讨，对植物化石夹层的碎屑岩进行了碎屑锆石LA-ICP-MS U-Pb年代学分析。
和盛植物群由18属31种组成，名单如下：Lepidophylloides sp.，Stigmariaficoides (Sternb.) Brongn.， Trizygia oblongifolium (Germ. et Kaulf.) Asama，Calamites cistii Brongn.，C. sp.，Paracalamites stenocostatus Gu et Zhi，Annulariastellata (Schloth.) Wood， A. sp.， Schizoneura sp.， Sphenopteridiumpseudogermanicum (Halle) Sze，Sphenopteris rotunda Sze，Pecopteris arborescens(Schloth.) Sternb.，P. candolleana Brongn.，P. cyathea (Schloth.) Brongn.，P.huichensis Hsü，P. marginata Gu et Zhi，P. cf. P.(Asterotheca) orientalis (Schenk)Pot.，P. yabei Kaw.，P. sp.，Neuropteris ovata Hoffm.，N. plicata Sternb.，Odontopterissubcrenulata (Rost) Zeill.，Emplectopteris cf. E.triangularis Halle，E. sp.(cf. E.sinensis Huang)，Taeniopteris cf. T. multinervis Weiss，T. yernauxii Stockm. et Math.，Cordaites principalis (Germ.) Gein.， C. schenkii Halle， Cardiocarpus sp.，Rhabdocarpus sp.，Radicites sp.。和盛植物群主要由真蕨与种子蕨纲以及楔叶纲分子组成；多数属种为华夏植物群的重要和常见分子，其中不乏标志或特有分子，如Emplectopteris，Taeniopteris yernauxii，Pecopteris huichensis，P. marginata等。和盛植物群具有华夏植物群性质，在古植物地理上属于华夏植物地理大区华北植物区。该植物群可以与以Emplectopteris triangularis—Emplectopteridium alatum为代表的早二叠世华夏植物群进行对比，其地质时代为亚丁斯克期—空谷期早期。
和盛植物群产出层位——和盛组是以灰色、灰黑色含砾砂岩、砂岩、粉砂岩及粉砂质泥岩为主的陆相沉积，属于上石炭—下二叠统山秀岭组海相碳酸盐岩沉积和下—中二叠统大蒜沟组海相碳酸盐岩及碎屑岩沉积之间的一套陆相碎屑岩沉积。该组的地质时代被其自身所含的植物化石和其上下层位中的海相化石（蜓）共同限定为早二叠世晚期（亚丁斯克期—空谷期早期）。
和盛组碎屑锆石年龄分布区间为2541—2535Ma、1897—1832Ma，458—452Ma，390—280Ma，测年结果约束的和盛组的最大沉积年龄为280Ma。支持了将和盛植物群与和盛组的时代定为亚丁斯克—空谷期早期的认识。物源分析结果表明和盛组物源来自华北板块，缺乏佳蒙地块的特征物源，说明早二叠世中—晚期延边汪清和盛地区仍属于华北板块，与佳蒙地块相距甚远。
结合古植物学、地层学、碎屑锆石年代学以及地球物理学等资料，提出华夏植物地理大区与安加拉植物地理大区的区系界线及索伦—西拉木伦河缝合带在延边地区的延伸位置应位于汪清—珲春一线。嘎呀河—图们江很可能为华北板块与佳蒙地块的主碰撞带的位置。
和盛植物群的发现和研究成果，不但提高了华夏植物群华北区的研究程度，将华夏植物群的分布范围向北扩展到汪清地区；而且较好地限定了延边地区华夏植物地理大区与安加拉植物地理大区的分界线，为恢复东北东部晚古生代地质历史、重建东北亚区域构造演化提供了重要的资料。
There existed four major phytogeographic realms namely the Cathaysia,Euramerica, Angara and Gondwana during the Carboniferous-Permian period in theworld. South part and north part of Northeast China developed respectively theCathaysia and the Angara floras, which boundary lies in the Xar Moron River.However, eastern extension of the boundary in eastern Northeast China is still unclear.The last decades have witnessed a growing debate in research on Paleozoicstratigraphy in Yanbian area, Jilin Province. Some scientists even hold the opinionthat Carboniferous-Permian is dominated by ophiolite complex and turbidite-mélange rocks. The problems mentioned above seriously affect to determine theeastern extension of the Solonker-Xar Moron River suture zone.
This thesis aims at fixing the boundary between Permian Cathaysia and Angaraflora in eastern Northeast China, ascertaining Paleozoic stratigraphic sequence inYanbian area, and confining the eastern extension of the Solonker-Xar Moron Riversuture. Systematic botany of a newly found Hesheng flora was done by the presentauthor and also the stratigraphy of fossil sites in the Daxinggou Town, WangqingCounty, Yanbian area, Jilin Province, NE China was investigated, and LA–ICP–MSU-Pb detrital zircon geochronology of clastic rocks from the fossil plants interbedewas analyzed. The results are as follows:
The fossil plants of the Hesheng flora consist of31species of18genera, namelyLepidophylloides sp., Stigmaria ficoides (Sternb.) Brongn., Trizygia oblongifolium(Germ. et Kaulf.) Asama, Calamites cistii Brongn., C. sp., Paracalamitesstenocostatus Gu et Zhi, Annularia stellata (Schloth.) Wood, A. sp., Schizoneura sp.,Sphenopteridium pseudogermanicum (Halle) Sze, Sphenopteris rotunda Sze,Pecopteris arborescens (Schloth.) Sternb., P. candolleana Brongn., P. cyathea(Schloth.) Brongn., P. huichensis Hsü, P. marginata Gu et Zhi, P. cf. P.(Asterotheca)orientalis (Schenk) Pot., P. yabei Kaw., P. sp., Neuropteris ovata Hoffm., N. plicataSternb., Odontopteris subcrenulata (Rost) Zeill., Emplectopteris cf. E.triangularisHalle, E. sp.(cf. E. sinensis Huang), Taeniopteris cf. T. multinervis Weiss, T.yernauxii Stockm. et Math., Cordaites principalis (Germ.) Gein., C. schenkii Halle,Cardiocarpus sp., Rhabdocarpus sp., Radicites sp. The Hesheng flora is dominated byferns and seed ferns. Most of the fossil plants are important or peculiar of theCathaysia flora, such as Emplectopteris, Taeniopteris yernauxii, Pecopteris huicensisand P. maginata. This indicates the Hesheng flora has a typical Cathaysia floristiccharacter and situate in North China Province of the Cathaysia realm. The Heshengflora, which is comparative to Early Permian Emplectopteris triangularis-Emplectopteridium alatum assembles of Shanxi Formation in North China andNorthwest China, is Late Cisuralian of Permian (Artinskian-early Kungurian) in age.
The plants fossil-bearing beds of the Hesheng Formation is of late Cisuralian(Artinskian-early Kungurian) in age. The formation consists of about230m of greyand dark grey conglomerate, coarse-grained sandstone, siltstone and mudstone, underlying by the Late Carboniferous–Early Permian marine carbonate of theShanxiuling Formation with an unconformable contact, and overlain by the Cisuralian-Guadalupian marine carbonate of the Dasuangou Formation.
The U-Pb ages of detrital zircon grains from the Hesheng Formation are dividedinto four groups:2541-2535Ma,1897-1832Ma,458-452Ma and390-280Ma.Constrained results from detrital zircon U-Pb geochronology of clastic rock prove thatages of the Hesheng flora and Hesheng Formation is younger than280Ma.Provenance analysis shows the clast came from the North China Plate and no sourcefrom Jiamusi-Mongolia Block. Therefore, Hesheng district of Wangqing County,Yanbian area belongs to North China Plate during middle-late Cisuralian.
Based on results of paleophytogeography, stratigraphy, detrital zircongeochronology and geophysical data, the boundary between Permian Cathaysia andAngara flora and the eastward extension of the Solonker-Xar Moron River sutureshould locate in the line of Wangqing-Hunchun in Yanbian area, Jilin Province.
The discovery of the Hesheng flora advances the research on Cathaysia flora inNorth China Province, and the distribution of the Cathaysia flora extends northwardto Wangqing district. This confines the boundary between the Cathaysia and Angarafloristic realms in eastern Northeast China, and provides significant data for Paleozoicgeology in Northeast China, and for research on regional tectonic evolution ofNortheast Asia.
为了确定东北东部二叠纪华夏植物群与安加拉植物群区系界线位置、查明延边地区地层发育序列、分析索伦—西拉木伦河缝合带在延边地区的延伸位置，本文首次对中国吉林省汪清县大兴沟镇和盛植物群进行了系统的古植物学研究，对植物化石产地进行了深入的地层学探讨，对植物化石夹层的碎屑岩进行了碎屑锆石LA-ICP-MS U-Pb年代学分析。
和盛植物群由18属31种组成，名单如下：Lepidophylloides sp.，Stigmariaficoides (Sternb.) Brongn.， Trizygia oblongifolium (Germ. et Kaulf.) Asama，Calamites cistii Brongn.，C. sp.，Paracalamites stenocostatus Gu et Zhi，Annulariastellata (Schloth.) Wood， A. sp.， Schizoneura sp.， Sphenopteridiumpseudogermanicum (Halle) Sze，Sphenopteris rotunda Sze，Pecopteris arborescens(Schloth.) Sternb.，P. candolleana Brongn.，P. cyathea (Schloth.) Brongn.，P.huichensis Hsü，P. marginata Gu et Zhi，P. cf. P.(Asterotheca) orientalis (Schenk)Pot.，P. yabei Kaw.，P. sp.，Neuropteris ovata Hoffm.，N. plicata Sternb.，Odontopterissubcrenulata (Rost) Zeill.，Emplectopteris cf. E.triangularis Halle，E. sp.(cf. E.sinensis Huang)，Taeniopteris cf. T. multinervis Weiss，T. yernauxii Stockm. et Math.，Cordaites principalis (Germ.) Gein.， C. schenkii Halle， Cardiocarpus sp.，Rhabdocarpus sp.，Radicites sp.。和盛植物群主要由真蕨与种子蕨纲以及楔叶纲分子组成；多数属种为华夏植物群的重要和常见分子，其中不乏标志或特有分子，如Emplectopteris，Taeniopteris yernauxii，Pecopteris huichensis，P. marginata等。和盛植物群具有华夏植物群性质，在古植物地理上属于华夏植物地理大区华北植物区。该植物群可以与以Emplectopteris triangularis—Emplectopteridium alatum为代表的早二叠世华夏植物群进行对比，其地质时代为亚丁斯克期—空谷期早期。
和盛植物群产出层位——和盛组是以灰色、灰黑色含砾砂岩、砂岩、粉砂岩及粉砂质泥岩为主的陆相沉积，属于上石炭—下二叠统山秀岭组海相碳酸盐岩沉积和下—中二叠统大蒜沟组海相碳酸盐岩及碎屑岩沉积之间的一套陆相碎屑岩沉积。该组的地质时代被其自身所含的植物化石和其上下层位中的海相化石（蜓）共同限定为早二叠世晚期（亚丁斯克期—空谷期早期）。
和盛组碎屑锆石年龄分布区间为2541—2535Ma、1897—1832Ma，458—452Ma，390—280Ma，测年结果约束的和盛组的最大沉积年龄为280Ma。支持了将和盛植物群与和盛组的时代定为亚丁斯克—空谷期早期的认识。物源分析结果表明和盛组物源来自华北板块，缺乏佳蒙地块的特征物源，说明早二叠世中—晚期延边汪清和盛地区仍属于华北板块，与佳蒙地块相距甚远。
结合古植物学、地层学、碎屑锆石年代学以及地球物理学等资料，提出华夏植物地理大区与安加拉植物地理大区的区系界线及索伦—西拉木伦河缝合带在延边地区的延伸位置应位于汪清—珲春一线。嘎呀河—图们江很可能为华北板块与佳蒙地块的主碰撞带的位置。
和盛植物群的发现和研究成果，不但提高了华夏植物群华北区的研究程度，将华夏植物群的分布范围向北扩展到汪清地区；而且较好地限定了延边地区华夏植物地理大区与安加拉植物地理大区的分界线，为恢复东北东部晚古生代地质历史、重建东北亚区域构造演化提供了重要的资料。
There existed four major phytogeographic realms namely the Cathaysia,Euramerica, Angara and Gondwana during the Carboniferous-Permian period in theworld. South part and north part of Northeast China developed respectively theCathaysia and the Angara floras, which boundary lies in the Xar Moron River.However, eastern extension of the boundary in eastern Northeast China is still unclear.The last decades have witnessed a growing debate in research on Paleozoicstratigraphy in Yanbian area, Jilin Province. Some scientists even hold the opinionthat Carboniferous-Permian is dominated by ophiolite complex and turbidite-mélange rocks. The problems mentioned above seriously affect to determine theeastern extension of the Solonker-Xar Moron River suture zone.
This thesis aims at fixing the boundary between Permian Cathaysia and Angaraflora in eastern Northeast China, ascertaining Paleozoic stratigraphic sequence inYanbian area, and confining the eastern extension of the Solonker-Xar Moron Riversuture. Systematic botany of a newly found Hesheng flora was done by the presentauthor and also the stratigraphy of fossil sites in the Daxinggou Town, WangqingCounty, Yanbian area, Jilin Province, NE China was investigated, and LA–ICP–MSU-Pb detrital zircon geochronology of clastic rocks from the fossil plants interbedewas analyzed. The results are as follows:
The fossil plants of the Hesheng flora consist of31species of18genera, namelyLepidophylloides sp., Stigmaria ficoides (Sternb.) Brongn., Trizygia oblongifolium(Germ. et Kaulf.) Asama, Calamites cistii Brongn., C. sp., Paracalamitesstenocostatus Gu et Zhi, Annularia stellata (Schloth.) Wood, A. sp., Schizoneura sp.,Sphenopteridium pseudogermanicum (Halle) Sze, Sphenopteris rotunda Sze,Pecopteris arborescens (Schloth.) Sternb., P. candolleana Brongn., P. cyathea(Schloth.) Brongn., P. huichensis Hsü, P. marginata Gu et Zhi, P. cf. P.(Asterotheca)orientalis (Schenk) Pot., P. yabei Kaw., P. sp., Neuropteris ovata Hoffm., N. plicataSternb., Odontopteris subcrenulata (Rost) Zeill., Emplectopteris cf. E.triangularisHalle, E. sp.(cf. E. sinensis Huang), Taeniopteris cf. T. multinervis Weiss, T.yernauxii Stockm. et Math., Cordaites principalis (Germ.) Gein., C. schenkii Halle,Cardiocarpus sp., Rhabdocarpus sp., Radicites sp. The Hesheng flora is dominated byferns and seed ferns. Most of the fossil plants are important or peculiar of theCathaysia flora, such as Emplectopteris, Taeniopteris yernauxii, Pecopteris huicensisand P. maginata. This indicates the Hesheng flora has a typical Cathaysia floristiccharacter and situate in North China Province of the Cathaysia realm. The Heshengflora, which is comparative to Early Permian Emplectopteris triangularis-Emplectopteridium alatum assembles of Shanxi Formation in North China andNorthwest China, is Late Cisuralian of Permian (Artinskian-early Kungurian) in age.
The plants fossil-bearing beds of the Hesheng Formation is of late Cisuralian(Artinskian-early Kungurian) in age. The formation consists of about230m of greyand dark grey conglomerate, coarse-grained sandstone, siltstone and mudstone, underlying by the Late Carboniferous–Early Permian marine carbonate of theShanxiuling Formation with an unconformable contact, and overlain by the Cisuralian-Guadalupian marine carbonate of the Dasuangou Formation.
The U-Pb ages of detrital zircon grains from the Hesheng Formation are dividedinto four groups:2541-2535Ma,1897-1832Ma,458-452Ma and390-280Ma.Constrained results from detrital zircon U-Pb geochronology of clastic rock prove thatages of the Hesheng flora and Hesheng Formation is younger than280Ma.Provenance analysis shows the clast came from the North China Plate and no sourcefrom Jiamusi-Mongolia Block. Therefore, Hesheng district of Wangqing County,Yanbian area belongs to North China Plate during middle-late Cisuralian.
Based on results of paleophytogeography, stratigraphy, detrital zircongeochronology and geophysical data, the boundary between Permian Cathaysia andAngara flora and the eastward extension of the Solonker-Xar Moron River sutureshould locate in the line of Wangqing-Hunchun in Yanbian area, Jilin Province.
The discovery of the Hesheng flora advances the research on Cathaysia flora inNorth China Province, and the distribution of the Cathaysia flora extends northwardto Wangqing district. This confines the boundary between the Cathaysia and Angarafloristic realms in eastern Northeast China, and provides significant data for Paleozoicgeology in Northeast China, and for research on regional tectonic evolution ofNortheast Asia.
引文
Asama K.1956. Permian Plants from Maiya in Northern Honshu, Japan. Proceedings of theJapan Academy73(7):469-471
Asama K.1967. Permian plants from Maiya, Japan,1. Cathaysiopteris and Psygmophyllum.Bulletin of the National Science Museum. Series C,10(2):139-153
Asama K.1970. Evolution and Classification of Sphenophyllales in Cathaysia Land. Bull. Nat.Sci. Mus.,13(2):291-317
Asama K.1974. Permian plants from Takakurayama. Bulletin of the National Science Museum.Series C,17(3):239-250
Asama K.1981. Permian Plants from Maiya, Japan2. Taeniopteris. Bulletin of the NationalScience Museum. Series C, Geology&paleontology,7(1):1-27
Asama K.1988. On some problems of paleogeography inferred from the Permian floras ofNortheast Japan. Earth Science,42(4):202-211
Asama K.1989. Permian Plants from Maiya, Japan,3. Pteriodophylls. Bulletin of the NationalScience Museum. Series C,15(2):39-52
Blakey R.2011. Global Paleogeography, http://jan.ucc.nau.edu/~rcb7/index.html
Celal Seng r A M.1990. Plate tectonics and orogenic research after25years: A Tethyanperspective. Earth-Science Reviews,27(1-2):1-201
Chen B, Jahn B M, Tian W.2009. Evolution of the Solonker suture zone: Constraints from zirconU-Pb ages, Hf isotopic ratios and whole-rock Nd-Sr isotope compositions of subduction-and collision-related magmas and forearc sediments. Journal of Asian Earth Sciences,34(3):245-257
Cope T, Ritts B D, Darby B J, Fildani A, Graham S A.2005. Late Paleozoic Sedimentation onthe Northern Margin of the North China Block: Implications for Regional Tectonics andClimate Change. International Geology Review,47(3):270-296
Deng S, Wan C, Yang J.2009. Discovery of a Late Permian Angara-Cathaysia mixed flora fromAcheng of Heilongjiang,China,with discussions on the closure of the Paleoasian Ocean.Science in China(Series D:Earth Sciences),52(11):1746-1755
Dobretsov N L, Buslov M M, Vernikovsky V A.2003. Neoproterozoic to Early OrdovicianEvolution of the Paleo-Asian Ocean: Implications to the Break-up of Rodinia.Gondwana Research,6(2):143-159
Enkin R J, Yang Z, Chen Y, Courtillot V.1992. Paleomagnetic Constraints on the GeodynamicHistory of the Major Blocks of China From the Permian to the Present. Journal ofGeophysical Research,97(B10):13953-13989
Ernst W G, Tsujimori T, Zhang R, Liou J G.2007. Permo-Triassic collision, subduction-zonemetamorphism, and tectonic exhumation along the east Asian continental margin.Annual Review of Earth and Planetary Sciences,35:73-110
Fedo C M, Sircombe K N, Rainbird R H.2003. Detrital Zircon Analysis of the SedimentaryRecord. Reviews in Mineralogy and Geochemistry,53(1):277-303
Grant M L, Wilde S A, Wu F, Yang J.2009. The application of zircon cathodoluminescenceimaging, Th-U-Pb chemistry and U-Pb ages in interpreting discrete magmatic andhigh-grade metamorphic events in the North China Craton at the Archean/Proterozoicboundary. Chemical Geology,261(1-2):155-171
Halle T G.1927. Palaeozoic plants from central Shansi. Peking: Geological survey of China.1-316
Halle T G.1935. On the distribution of the Late Palaeozoic floras in Asia. Geografiska Annaler,17:106-111
Jia D, Hu R, Lu Y, Qiu X.2004. Collision belt between the Khanka block and the North Chinablock in the Yanbian Region, Northeast China. Journal of Asian Earth Sciences,23(2):211-219
Jian P, Kr ner A, Windley B F, Shi Y, Zhang W, Zhang L, Yang W.2012. Carboniferous andCretaceous mafic–ultramafic massifs in Inner Mongolia (China): A SHRIMP zircon andgeochemical study of the previously presumed integral―Hegenshan ophiolite‖. Lithos,142–143(0):48-66
Kawasaki S.1927. The Flora of the Heian System, Pt.1. Bull. Geol. Surv. of Chosen,6(1-2):1-30, pls.31-99
Kawasaki S.1934. The Flora of the Heian System, Pt.2. Bull. Geol. Surv. of Chosen,6(4):47-311, pls.105-110
Kawasaki S, Konno E.1932. The Flora of the Heian System, Pt.3. Bull. Geol. Surv. of Chosen,6(3):31-44,61-279, pls.100-104
Khain E V, Bibikova E V, Kr ner A, Zhuravlev D Z, Sklyarov E V, Fedotova A A,Kravchenko-Berezhnoy I R.2002. The most ancient ophiolite of the Central Asian foldbelt: U-Pb and Pb-Pb zircon ages for the Dunzhugur Complex, Eastern Sayan, Siberia,and geodynamic implications. Earth and Planetary Science Letters,199(3-4):311-325
Khain E V, Bibikova E V, Salnikova E B, Kr ner A, Gibsher A S, Didenko A N, Degtyarev K E,Fedotova A A.2003. The Palaeo-Asian ocean in the Neoproterozoic and earlyPalaeozoic: new geochronologic data and palaeotectonic reconstructions. PrecambrianResearch,122(1-4):329-358
Kon'no E.1960. Schizoneura manchuriensis Kon'no and its Fructification (Manchurostachys n.gen.) from the Gigantopteris-nicotianaefolia-bearing Formation in Penchihu Coal-field,Northeastern China. Science Reports, Tohoku University, Sendai, Japan, Spec. Vol.(4):163-188
Kon'no E.1968. The Upper Permian Flora from the Eastern Border of Northeast China. ScienceReports of the Tohoku University, second series (Geology),39(3):159-211, pls.111-125
Koschek G.1993. Origin and significance of the SEM cathodoluminescence from zircon. Journalof Microscopy,171(3):223-232
Kotlyar G V, Belyansky G C, Burago V I, Nikitina A P, Zakharov Y D, Zhuravlev A V.2006.South Primorye, Far East Russia—A key region for global Permian correlation. Journalof Asian Earth Sciences,26(3-4):280-293
Lee D.1987. Geology of Korea. Seoul: The Kyohak-sa Publishing Co.1-514
Li D, Chen Y, Wang Z, Hou K, Liu C.2011a. Detrital zircon U-Pb ages, Hf isotopes and tectonicimplications for Palaeozoic sedimentary rocks from the Xing-Meng orogenic belt,middle-east part of inner Mongolia, China. Geological Journal,46(1):63-81
Li H, Xu Y, Huang X, He B, Luo Z, Yan B.2009. Activation of northern margin of the NorthChina Craton in Late Paleozoic: Evidence from U-Pb dating and Hf isotopes of detritalzircons from the Upper Carboniferous Taiyuan Formation in the Ningwu-Jingle basin.Chinese Science Bulletin,54(4):677-686
Li J Y.2006. Permian geodynamic setting of Northeast China and adjacent regions: closure ofthe Paleo-Asian Ocean and subduction of the Paleo-Pacific Plate Journal of Asian EarthSciences,26(3-4):207-224
Li S Z, Zhao G C, Santosh M, Liu X, Dai L M.2011b. Palaeoproterozoic tectonothermalevolution and deep crustal processes in the Jiao-Liao-Ji Belt, North China Craton: areview. Geological Journal,46(6):525-543. doi:10.1002/gj.1282
Li W, Zhong R, Xu C, Song B, Qu W.2012. U–Pb and Re–Os geochronology of the BainaimiaoCu–Mo–Au deposit, on the northern margin of the North China Craton, Central AsiaOrogenic Belt: Implications for ore genesis and geodynamic setting. Ore GeologyReviews, In press. doi:10.1016/j.oregeorev.2012.03.001
Li X, Wu X.1996. Late paleozoic phytogeographic provinces in China and its adjacent regions.Review of Palaeobotany and Palynology,90(1-2):41-62
Liu L J, Wang X F, Yao Z Q.1996. Emplectopteris and allied pteridosperms from the KaipingBasin, China. Palaeontographica Abt B,239:109-136
Lu X-P, Wu F-Y, Guo J-H, Wilde S A, Yang J-H, Liu X-M, Zhang X-O.2006. Zircon U-Pbgeochronological constraints on the Paleoproterozoic crustal evolution of the Easternblock in the North China Craton. Precambrian Research,146(3-4):138-164
Luo Y, Sun M, Zhao G, Li S, Xu P, Ye K, Xia X.2004. LA-ICP-MS U-Pb zircon ages of theLiaohe Group in the Eastern Block of the North China Craton: constraints on theevolution of the Jiao-Liao-Ji Belt. Precambrian Research,134(3-4):349-371
Markevich P V, Zakharov Y D.2008. Triassic and Jurassic of the Sikhote-Alin:Volcano-Sedimentary assemblage, Paleobiogeography (in Russian). Vladivostok:Dalnauka.1-299
McElhinny M W, Embleton B J J, Ma X H, Zhang Z K.1981. Fragmentation of Asia in thePermian. Nature,293(5829):212-216
Mei M, Huang Q C, Du M, Dilcher D L.1996. The Xu-Huai-Yu Subprovince of the CathaysianFloral Province. Review of Palaeobotany and Palynology,90(1-2):63-77
Meng E, Xu W-L, Pei F-P, Yang D-B, Yu Y, Zhang X-Z.2010. Detrital-zircon geochronology ofLate Paleozoic sedimentary rocks in eastern Heilongjiang Province, NE China:Implications for the tectonic evolution of the eastern segment of the Central AsianOrogenic Belt. Tectonophysics,485(1-4):42-51
Naugolnykh S V.2002. Paracalamitina striata--a Newly Reconstructed Equisetophyte from thePermian of Angaraland. Journal of Paleontology,76(2):377-385
Seyfullah L J, Hilton J.2009. Re-evaluation of Halle's fertile pteridosperms from the Permianfloras of Shanxi Province, China. Plant Systematics and Evolution,279(1-4):191-218
Seyfullah L J, Hilton J.2011. Callistophytalean pteridosperms from Permian aged floras ofChina. Palaeontology,54(2):287-302
Shen S-Z, Zhang H, Shang Q H, Li W-Z.2006. Permian stratigraphy and correlation ofNortheast China: A review. Journal of Asian Earth Sciences,26(3-4):304-326
Shi G R.2006. The marine Permian of East and Northeast Asia: an overview of biostratigraphy,palaeobiogeography and palaeogeographical implications. Journal of Asian EarthSciences,26(3-4):175-206
Stockmans F, Mathieu F-F.1939. La Flore Paleozoique du Bassin Houiller de Kaiping (Chine).Bruxelles.49-165, pls.161-134
Stockmans F, Mathieu F-F.1957. La Flore Paleozoique du Bassin Houiller de Kaiping(Chine)(Deuxieme Partie). Bruxelles.1-89, pls.81-15
Sun K-Q.2006. The Cathaysia Flora and the Mixed Late Permian Cathaysian-Angaran Floras inEast Asia. Journal of Integrative Plant Biology,48(4):381-389
Wang C-w, Sun Y-w, Li N, Zhao G-w, Ma X-q.2009. Tectonic implications of Late Paleozoicstratigraphic distribution in Northeast China and adjacent region. Science in ChinaSeries D-Earth Sciences,52(5):619-626
Wang C, Li N, Sun Y, Zong P.2011. Distribution of Tuvaella Brachiopod Fauna and its tectonicSignificance. Journal of Earth Science,22(1):11-19
Wang J.2010. Late Paleozoic macrofloral assemblages from Weibei Coalfield, with reference tovegetational change through the Late Paleozoic Ice-age in the North China Block.International Journal of Coal Geology,83(2-3):292-317
Wang J, Pfefferkorn H W, Zhang Y, Feng Z.2012. Permian vegetational Pompeii from InnerMongolia and its implications for landscape paleoecology and paleobiogeography ofCathaysia. Proceedings of the National Academy of Sciences,109(13):4927-4932. doi:10.1073/pnas.1115076109
Wilde S A, Valley J W, Peck W H, Graham C M.2001. Evidence from detrital zircons for theexistence of continental crust and oceans on the Earth4.4Gyr ago. Nature,409(6817):175-178
Wilde S A, Wu F-Y, Zhao G.2010. The Khanka Block, NE China, and its significance for theevolution of the Central Asian Orogenic Belt and continental accretion. GeologicalSociety, London, Special Publications,338:117-137
Wu F-Y, Sun D-Y, Ge W-C, Zhang Y-B, Grant M L, Wilde S A, Jahn B-M.2011. Geochronologyof the Phanerozoic granitoids in northeastern China. Journal of Asian Earth Sciences,41(1):1-30
Wu F-Y, Yang J-H, Lo C-H, Wilde S A, Sun D-Y, Jahn B-M.2007a. The Heilongjiang Group: AJurassic accretionary complex in the Jiamusi Massif at the western Pacific margin ofnortheastern China. Island Arc,16(1):156-172
Wu F-Y, Yang J-H, Wilde S A, Liu X-M, Guo J-H, Zhai M-G.2007b. Detrital zircon U-Pb andHf isotopic constraints on the crustal evolution of North Korea. Precambrian Research,159(3-4):155-177
Wu F-Y, Zhao G-C, Sun D-Y, Wilde S A, Yang J-H.2007c. The Hulan Group: Its role in theevolution of the Central Asian Orogenic Belt of NE China. Journal of Asian EarthSciences,30(3-4):542-556
Xiao W J, Windley B F, Hao J, Zhai M G.2003. Accretion leading to collision and the PermianSolonker suture, Inner Mongolia, China: Termination of the central Asian orogenic belt.Tectonics,22(6),1069. doi:10.1029/2002TC001484
Xu X, Harbert W, Dril S, Kravchinksy V.1997. New paleomagnetic data from theMongol-Okhotsk collision zone, Chita region, south-central Russia: implications forPaleozoic paleogeography of the Mongol-Okhotsk ocean. Tectonophysics,269(1-2):113-129
Yang J-H, Wu F-Y, Shao J-A, Wilde S A, Xie L-W, Liu X-M.2006. Constraints on the timing ofuplift of the Yanshan Fold and Thrust Belt, North China. Earth and Planetary ScienceLetters,246(3-4):336-352
Zhang S H, Zhao Y, Song B, Yang Z Y, Hu J M, Wu H.2007. Carboniferous granitic plutonsfrom the northern margin of the North China block: implications for a late Palaeozoicactive continental margin. Journal of the Geological Society,164(2):451-463
Zhang Y, Wu F, Wilde S A, Zhai M, Lu X, Sun D.2004. Zircon U-Pb ages and tectonicimplications of 'Early paleozoic' granitoids at Yanbian, Jilin Province, northeast china.Island Arc,13(4):484-505
Zhang Y, Wu F, Zhai M, Lu X.2005. Tectonic setting of the Helong Block: Implications for thenorthern boundary of the eastern North China Craton. Science in China Ser. D EarthSciences,48(10):1599-1612
Zhao G, Sun M, Wilde S A, Sanzhong L.2005. Late Archean to Paleoproterozoic evolution ofthe North China Craton: key issues revisited. Precambrian Research,136(2):177-202
Zhao G, Wilde S A, Cawood P A, Sun M.2001. Archean blocks and their boundaries in the NorthChina Craton: lithological, geochemical, structural and P-T path constraints and tectonicevolution. Precambrian Research,107(1-2):45-73
Zhao X, Coe R S.1987. Paleomagnetic constraints on the collision and rotation of North andSouth China. Nature,327(6118):141-144
Zhao X, Coe R S, Yaoxiu Z, Haoruo W, Jie W.1990. New paleomagnetic results from northernChina: collision and suturing with Siberia and Kazakhstan. Tectonophysics,181(1-4):43-81
Zhou J-B, Wilde S A, Zhang X-Z, Zhao G-C, Liu F-L, Qiao D-W, Ren S-M, Liu J-H.2011. A>1300km late Pan-African metamorphic belt in NE China: New evidence from theXing'an block and its tectonic implications. Tectonophysics,509(3-4):280-292
Zhou J-B, Wilde S A, Zhang X-Z, Zhao G-C, Zheng C-Q, Wang Y-J, Zhang X-H.2009. Theonset of Pacific margin accretion in NE China: Evidence from the Heilongjianghigh-pressure metamorphic belt. Tectonophysics,478(3-4):230-246
Boucot A J,陈旭, Scotese C R,樊隽轩.2009.显生宙全球古气候重建.北京:科学出版社.1-173
陈旭,阮亦萍,布科AJ.2001.中国古生代气候演变.北京:科学出版社.1-325
窦亚伟,孙喆华,吴绍祖,顾道源.1983.西北地区古生物图册新疆维吾尔自治区分册（二）（晚古生代）.北京:地质出版社.561-614
耿元生,沈其韩,任留东.2010.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,26(7):1945-1966
郭孟习,孙炜,尹国义,彭玉鲸.2000.郯庐断裂系的北延及地质-地球物理特征.吉林地质,19(3):35-44
郭胜哲,苏养正,池永一,黄本宏.1992.吉林、黑龙江东部地槽区古生代生物地层及岩相古地理.见:南润善,郭胜哲编.内蒙古-东北地槽区古生代生物地层及古地理.北京:地质出版社.71-146
郭晓丹,周建波,张兴洲,邱海峻.2011.内蒙古西乌珠穆沁旗本巴图组碎屑锆石LA-ICP-MS U-Pb年龄及其意义.地质通报,30(Z1):278-290
Gu et Zhi.1974.中国植物化石：第一册，中国古生代植物.北京:科学出版社.1-277
韩江,聂立军.2003.吉林省延边开山屯地区大蒜沟组生物化石的发现及其意义.吉林地质,22(3):19-23
韩杰,周建波,张兴洲,邱海峻.2011.内蒙古林西地区上二叠统林西组砂岩碎屑锆石的年龄及其大地构造意义.地质通报,30(Z1):258-269
何锡麟,梁敦士,沈树忠.1996.中国江西二叠纪植物群研究.徐州:中国矿业大学出版社.1-300
何锡麟,朱梅丽,范炳恒,庄寿强,丁惠,薛庆远.1995.山西太原东山晚古生代地层划分对比及古生物研究.长春:吉林大学出版社.1-149, pls.141-172
黑龙江地质矿产局.1993.黑龙江省区域地质志.北京:地质出版社:1-734
黄本宏.1976.华北地区古生物图册内蒙古分册（一）古生代部分.北京:地质出版社.355-379
黄本宏.1977.小兴安岭东南部二叠纪植物群.北京:地质出版社.1-79
黄本宏.1980.古植物.见:沈阳地质矿产研究所编.东北地区古生物图册（一）古生代分册.北京:地质出版社.522-573
黄本宏.1982.东北北部石炭二叠纪陆相地层及古地理概况.地质论评,28(5):395-402
黄本宏.1983.天山-兴安褶皱区东部古生代末植物地理区系及其地质意义.见:唐克东编.中国北方板块构造文集(第一集).138-155
黄本宏.1986a.华夏植物群特有植物——织羊齿(Emplectopteris).中国地质科学院沈阳地质矿产研究所所刊,(14):137-145
黄本宏.1986b.内蒙古镶黄旗地区早二叠世植物化石.见:唐克东编.中国北方板块构造论文集.北京:地质出版社:115-135
黄本宏.1987.辽宁省东部及南部中、晚石炭世地层及植物化石.中国地质科学院沈阳地质矿产研究所所刊,15:43-76
黄本宏.1993.大兴安岭地区石炭、二叠系及植物群.北京:地质出版社.1-141
黄本宏.1995.安加拉植物群在我国石炭纪、二叠纪的分布及其与华夏植物群的关系.见:李星学编.中国地质时期植物群.广州:广东科技出版社.174-189
黄本宏.1997.长白山地晚古生代地层及植物群.中国地质科学院沈阳地质矿产研究所集刊,(5-6):185-268
黄本宏.2000.内蒙古高原晚古生代植物群.植物学通报,17(专辑):172-178
黄汲清,任纪舜,姜春发,张正坤,秦德余.1980.中国大地构造及其演化——1:400万中国大地构造图简要说明.北京:科学出版社.1-124
黄联盟,黄玉宁,梅美堂,李生盛.1989.闽西南早二叠世含煤地层及植物群.北京:煤炭工业出版社.1-101
吉林省地质局第四地质队.1966.1/20万《大兴沟幅》K-52-Ⅳ区域地质测量报告书.长春:吉林省地质局.1-59
吉林省地质局区域地质测量大队.1978.1/20万《敦化县幅》K-52-3区域地质调查报告（地质部分）.长春:吉林省地质局.1-213
吉林省地质局区域地质测量大队第二分队.1965.1/20万《大拉子幅》K-52-ⅩⅥ区域地质测量报告书（地质部分）.长春:吉林省地质局.1-100
吉林省地质局区域地质测量大队第三分队.1965.1/20万《珲春幅》K-52-11，《春化幅》K-52-12区域地质测量报告书.长春:吉林省地质局.1-36
吉林省地质矿产局.1988.吉林省区域地质志.北京:地质出版社.1-698
吉林省区域地层表编写组.1978.东北地区区域地层表吉林省分册.北京:地质出版社.1-214
今野圓蔵.1947.滿洲本溪湖炭田及間島省開山屯附近の二疊系の層序學的並に古植物學的研究.地質學雜誌,53(622-627):102-103
金建华,杜小弟.1993.小兴安岭东南部晚二叠世地层新认识.煤田地质与勘探,21(3):7-12
金玉玕,王向东,尚庆华,王玥,盛金章.1999.中国二叠纪年代地层划分和对比.地质学报,73(2):97-108
寇晓威.1994.吉林省大黑山条垒中部早二叠世地层的发现及其意义.吉林地质,13(1):35-41
郎嘉彬,王成源.2010.吉林磐石地区鹿圈屯组的牙形刺.吉林大学学报(地球科学版),40(3):603-609
李春昱.1980.中国板块构造的轮廓.中国地质科学院院报,2(1):11-22
李春昱,王荃.1983.我国北部边陲及邻区的古板块构造与欧亚大陆的形成.见:唐克东编.中国北方板块构造文集(第一集).3-17
李东津.1997.吉林省岩石地层.武汉:中国地质大学出版社.1-324
李锦轶.1986.内蒙古东部中朝板块与西伯利亚板块之间古缝合带的初步研究.科学通报,(14):1093-1096
李明松,孙跃武,葛文春,张彦龙.2011a.吉林延边地区开山屯植物群的时代——碎屑锆石U-Pb年代学约束编.中国古生物学会第26届学术年会论文摘要集.贵州关岭.99-100
李明松,孙跃武,赵国伟.2011b.吉林延边地区汪清县大兴沟早二叠世华夏植物群的发现及其地质意义.地球科学进展,26(3):339-346
李双林,欧阳自远.1998.兴蒙造山带及邻区的构造格局与构造演化.海洋地质与第四纪地质,18(3):45-54
李星学.1963.华北月门沟群植物化石.北京:科学出版社.1-185
李星学.1980.东亚华夏植物群的鳞木类植物.中国科学,(2):166-171
李星学.1995.中国地质时期植物群.广州:广东科技出版社.1-542
李星学,沈光隆,田宝霖,王士俊,欧阳舒.1995.我国石炭纪、二叠纪植物群的几个论题.见:李星学编.中国地质时期植物群.广州:广东科技出版社.190-226
李星学,姚兆奇.1983.东亚石炭纪和二叠纪植物地理分区.见:古生物学基础理论丛书编委会编.中国古生物地理区系.北京:科学出版社.74-82
李忠,彭守涛,许承武,韩银学,翟明国.2009.韩国太白山盆地古生界砂岩碎屑锆石U-Pb年代及其区域构造含义.岩石学报,25(1):182-192
刘爱,张川波,文琼英.1994.吉林省“槽区”二叠系岩相古地理再造:未出版.1-144
刘爱，赵成弼.1998.延边石炭二叠系一个新的重要植物化石层位的发现.吉林地质:82
刘洪筹,沈光隆.1978.甘肃龙首山石炭纪和二叠纪植物群.兰州:兰州大学.1-152,pls.151-148
马醒华,邢历生,杨振宇,徐树金,张景鑫.1993.鄂尔多斯盆地晚古生代以来古地磁研究.地球物理学报,36(1):68-79
马醒华,杨振宇.1993.中国三大地块的碰撞拼合与古欧亚大陆的重建.地球物理学报,36(4):476-488
梅因C B,姚兆奇编译.1991.欧亚大陆古生代植物群和植物地理学.南京:南京大学出版社.1-177
米家榕,刘茂强.1985.吉林桦甸早二叠世大河深组的心脉羊齿(Cardioneura)古生物学报,24(6):618-624
彭玉鲸.1996.吉林省石炭-二叠纪生物地理区的划分.吉林地质,15(1):12-18
彭玉鲸.1997.解放村植物群的特征及其大地构造意义.吉林地质科技情报,(1):2-8
彭玉鲸,陈跃军,殷长建,李睿.2005.吉黑造山带古生代地层与混杂岩.世界地质,24(1):24-29
彭玉鲸,刘爱,李文国,赵成弼.1999.吉林省延边地区二叠纪的三类植物群与古陆缘再造.吉林地质,18(1):1-23
任纪舜,陈廷愚,牛宝贵,刘志刚,刘凤仁.1990.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.1-205
任纪舜,王作勋,陈炳蔚,姜春发,牛宝贵,李锦轶,谢广连,和政军,刘志刚.1999.从全球看中国大地构造：中国及邻区大地构造图简要说明.北京:地质出版社.1-50
邵济安,唐克东.1995.吉林省延边开山屯地区蛇绿混杂岩.岩石学报,11(增刊):212-220
邵济安,唐克东,詹立培,李子舜,徐公愉,王成源.1995.一个古大陆边缘的再造及其大地构造意义——延边地质研究新进展.中国科学(B辑化学生命科学地学),25(5):548-555
沈光隆.1995.二叠纪植物群.见:李星学编.中国地质时期植物群.广州:广东科技出版社.94-173
石新增.1985.吉林省二叠纪植物地理分区的点滴认识.吉林地质,4(2):47-52
斯行健.1989.内蒙古清水河及山西河曲晚古生代植物群.北京:科学出版社.1-268
宋彪,张玉海,万渝生,简平.2002.锆石SHRIMP样品靶制作、年龄测定及有关现象讨论.地质论评,48(增刊):26-30
孙柏年,沈光隆,刘燕学.1993.新疆塔里木盆地北缘的陆相下二叠统.兰州大学学报,29(1):110-115
孙德有,吴福元,张艳斌,高山.2004.西拉木伦河-长春-延吉板块缝合带的最后闭合时间———来自吉林大玉山花岗岩体的证据.吉林大学学报(地球科学版),34(2):174-181
孙革.1991.山西保德早二叠世Cordaites baodeensis sp. nov.叶表皮构造及Cordaites分类探讨.古生物学报,30(2):167-185
孙革.1993.中国吉林天桥岭晚三叠世植物群.长春:吉林科学技术出版社.1-157
孙革,赵衍华.1992.古生代植物.见:吉林省地质矿产局编.吉林省古生物图册.长春:吉林科技出版社.504-562
孙恒元.1984.吉林省延边地区晚石炭世的蜓类化石带.吉林地质,3(3):38-44
孙恒元.1988.吉林延边地区二叠系研究的进展.地层学杂志,12(3):202-229
孙恒元.1990.吉林延边地区二叠系大蒜沟组蜓类化石.微体古生物学报,7(3):257-264
孙克勤.1992.山东淄博地区晚石炭世和早二叠世植物群、古生态及沉积环境.长春:吉林大学出版社.1-143
孙克勤,邓胜徽.2003.贺兰山北段石炭纪和二叠纪植物群.现代地质,(03):259-267,357-358
孙克勤,张周良,阴家润,胡善亭.1996.贺兰山北段晚石炭世和早二叠世植物群古生态研究.现代地质,10(3):25-33
孙晓猛,王书琴,王英德,杜继宇,许强伟.2010.郯庐断裂带北段构造特征及构造演化序列.岩石学报,26(1):165-176
孙跃武,李明松,赵国伟.2012.吉林延边地区早二叠世一个新的陆相地层单位.地层学杂志,36(1):89-96
唐克东.1989.中朝陆台北侧褶皱带构造发展的几个问题.现代地质,3(2):195-204
唐克东,邵济安,李景春,康庄.2004.吉林延边缝合带的性质与东北亚构造.地质通报,23(9-10):885-891
唐克东,赵爱林.2007.吉林延边开山屯地区地层时代的新证据.地层学杂志,31(2):141-150
万天丰.2004.中国大地构造学纲要.北京:地质出版社.1-387
万天丰,朱鸿.1996.郯庐断裂带的最大左行走滑断距及其形成时期.高校地质学报,2(1):14-27
万天丰,朱鸿,赵磊,林建平,程捷,陈进.1996.郯庐断裂带的形成与演化：综述.现代地质,10(2):159-168
王成文,金巍,张兴洲,马志红,迟效国,刘永江,李宁.2008.东北及邻区晚古生代大地构造属性新认识.地层学杂志,32(2):119-136
王成文,孙跃武,李宁,刘欢,赵国伟.2009.东北地区晚古生代地层分布规律.地层学杂志,33(1):56-61
王鸿祯.1981.从活动论观点论中国大地构造分区.地球科学,(1):42-66
王鸿祯.1982.中国地壳构造发展的主要阶段.地球科学,18(3):155-178
王鸿祯.1985.中国古地理图集.北京:地图出版社.1-143
王鸿祯,刘本培.1981.中国中元古代以来古地理发展的轮廓.地层学杂志,5(2):77-89
王小凤,李中坚,陈柏林,陈宣华,董树文,张青,武红岭,邢历生,张宏,董法先,邬华梅,霍光辉,林传勇,白嘉启,刘晓春.2000.郯庐断裂带.北京:地质出版社.1-374
王玉净,樊志勇.1997.内蒙古西拉木伦河北部蛇绿岩带中二叠纪放射虫的发现及其地质意义.古生物学报,36(1):58-69
王钰,卢衍豪,杨敬之,穆恩之,盛金章.1954.辽东太子河流域地层(Ⅱ).地质学报,34(2):89-145
吴秀元,孙柏年,沈光隆,王永栋.1997.塔里木盆地北缘二叠纪植物群.古生物学报,36(S1):3-26
徐嘉炜.1980.郯—庐断裂带巨大的左行平移运动.合肥工业大学学报,(1):1-26+127-128
徐嘉炜.1985.郯庐断裂带北段平移研究的若干进展——答乔秀夫的“对郯庐断裂巨大平移质疑”.地质论评,31(1):83-86
徐嘉炜,崔可锐,刘庆,童蔚欣,朱光.1985.东亚大陆边缘中生代的左行平移断裂作用.海洋地质与第四纪地质,5(2):51-64
徐嘉炜,马国锋.1992.郯庐断裂带研究的十年回顾.地质论评,38(4):316-324
徐永文,贾连镇.1983.1/20万《珲春县幅》K-52-11，《春化幅》K-52-12，《敬信公社幅》K-52-17区域地质调查报告(地质部分).长春:吉林省地质矿产局区域地质调查大队.1-272
徐永文,殷长建.1991.1/5万《后河幅》K-52-19-D，《大兴沟镇幅》K-52-20-C区域地质调查报告：地质部分.长春:吉林省地质矿产局区域地质矿产调查所.1-186
阎同生,杨遵仪.2001.河北抚宁、曲阳晚古生代地层及植物群.北京:地质出版社.1-89
杨关秀,陈钟惠,张守良.1983.内蒙古准格尔旗东部太原组、山西组植物群特征.地球科学,(4):69-83,168-171
杨关秀等.2006.中国豫西二叠纪华夏植物群——禹州植物群.北京:地质出版社.1-361
杨涛.2010.吉林珲春晚二叠世解放村植物群.吉林大学,博士:1-101
叶茂,张世红,吴福元.1994.中国满洲里－绥芬河地学断面域古生代构造单元及其地质演化.长春地质学院学报,24(3):241-245
殷长建,孙春林,彭玉鲸,周晓东,赵衍华.2003.敦化隆起东缘晚石炭—早二叠世华夏植物群的发现及其地质意义.吉林大学学报(地球科学版),33(3):257-262
昝淑芹,高嘉瑞.1994.敦化-密山断裂带的特征、演化及与郯-庐断裂的关系.北京:地震出版社.52-57
张泓.1988.安加拉古陆外围晚二叠世混生植物群特征及形成机制的讨论.地质论评,34(4):343-350
张炯飞.1997.延边地区渤海地块与兴凯地块之间古缝合带的初步研究.吉林地质,16(2):30-37
张炯飞,张允平.1995.关于延边地区石炭-二叠系.中国地质科学院沈阳地质矿产研究所集刊,4:1-7
张开均.1998.华北板块东缘晚古生代火山活动及其大地构造含义.中国煤田地质,10(3):10-11,20
张理刚.1992.中国东部岩石圈铅同位素化学结构与动力学研究.矿物岩石地球化学通讯,11(3):133-137
张梅生,彭向东,孙晓猛.1998.中国东北区古生代构造古地理格局.辽宁地质,(2):12-17
张善桢,孙革,赵衍华.1987.吉林磐石吉昌地区早石炭世植物研究初报.古生物学报,26(4):456-470
张晓晖,翟明国.2010.华北北部古生代大陆地壳增生过程中的岩浆作用与成矿效应.岩石学报,26(5):1329-1341
张兴洲,穆石敏,杨宝俊,迟晓国.1999.拼合的大陆板块.见:张贻侠,孙运生,张兴洲,杨宝俊编.中国满洲里-绥芬河地学断面1：1000000说明书.北京:地质出版社.6-19
张兴洲,周建波,孙跃武,张凤旭,刘永江,朱占平,彭晓蕾,赵庆英,郎嘉彬,张淑芹,温泉波,迟效国,葛文春.2012.松辽盆地及外围上古生界石油地质综合研究2011年度中期工作报告.长春:吉林大学.
张宜.2009.山西保德晚古生代植物群.中国科学院南京地质古生物研究所,博士:1-157
张永焕,彭玉鲸,欧祥喜.2000.关于吉林省延边地区二叠纪地层的思考.吉林地质,19(1):1-12
赵春荆,彭玉鲸,党增欣,等.1996.吉黑东部构造格架及地壳演化.沈阳:辽宁大学出版社.1-186
赵修祜,刘陆军,侯吉辉.1987.晋东南地区晚古生代含煤地层和古生物群.南京:南京大学出版社.61-137
赵修祜,莫壮观,张善桢,姚兆奇.1980.黔西滇东晚二叠世植物群编.黔西滇东晚二叠世含煤地层和古生物群.北京:科学出版社.70-122
赵英利,刘永江,韩国卿,温泉波,李伟,梁道俊.2009.敦-密断裂左行走滑三维有限元模拟.世界地质,28(3):310-317
針尾慶次,川越浩.1923.間島豆滿江沿岸地質調查報告.南滿洲鐵道株式會社地質調查所.1-23
中国地质科学院地质研究所,新疆地矿局地质科学研究所.1986.新疆吉木萨尔大龙口二叠三叠纪地层及古生物群.北京:地质出版社.1-262
周晓东.2009.吉林省中东部地区下石炭统—下三叠统地层序列及构造演化.吉林大学,博士:1-103
周晓东,殷长建,彭玉鲸.2009.吉林延边地区柯岛群之由来及再认识.世界地质,28(1):37-44
朱光,宋传中,王道轩,刘国生,徐嘉炜.2001.郯庐断裂带走滑时代的40Ar/39Ar年代学研究及其构造意义.中国科学（D辑）,31(3):250-256
朱彤.1990.福建二叠纪含煤地层及古生物群.北京:地质出版社.1-127
Asama K.1967. Permian plants from Maiya, Japan,1. Cathaysiopteris and Psygmophyllum.Bulletin of the National Science Museum. Series C,10(2):139-153
Asama K.1970. Evolution and Classification of Sphenophyllales in Cathaysia Land. Bull. Nat.Sci. Mus.,13(2):291-317
Asama K.1974. Permian plants from Takakurayama. Bulletin of the National Science Museum.Series C,17(3):239-250
Asama K.1981. Permian Plants from Maiya, Japan2. Taeniopteris. Bulletin of the NationalScience Museum. Series C, Geology&paleontology,7(1):1-27
Asama K.1988. On some problems of paleogeography inferred from the Permian floras ofNortheast Japan. Earth Science,42(4):202-211
Asama K.1989. Permian Plants from Maiya, Japan,3. Pteriodophylls. Bulletin of the NationalScience Museum. Series C,15(2):39-52
Blakey R.2011. Global Paleogeography, http://jan.ucc.nau.edu/~rcb7/index.html
Celal Seng r A M.1990. Plate tectonics and orogenic research after25years: A Tethyanperspective. Earth-Science Reviews,27(1-2):1-201
Chen B, Jahn B M, Tian W.2009. Evolution of the Solonker suture zone: Constraints from zirconU-Pb ages, Hf isotopic ratios and whole-rock Nd-Sr isotope compositions of subduction-and collision-related magmas and forearc sediments. Journal of Asian Earth Sciences,34(3):245-257
Cope T, Ritts B D, Darby B J, Fildani A, Graham S A.2005. Late Paleozoic Sedimentation onthe Northern Margin of the North China Block: Implications for Regional Tectonics andClimate Change. International Geology Review,47(3):270-296
Deng S, Wan C, Yang J.2009. Discovery of a Late Permian Angara-Cathaysia mixed flora fromAcheng of Heilongjiang,China,with discussions on the closure of the Paleoasian Ocean.Science in China(Series D:Earth Sciences),52(11):1746-1755
Dobretsov N L, Buslov M M, Vernikovsky V A.2003. Neoproterozoic to Early OrdovicianEvolution of the Paleo-Asian Ocean: Implications to the Break-up of Rodinia.Gondwana Research,6(2):143-159
Enkin R J, Yang Z, Chen Y, Courtillot V.1992. Paleomagnetic Constraints on the GeodynamicHistory of the Major Blocks of China From the Permian to the Present. Journal ofGeophysical Research,97(B10):13953-13989
Ernst W G, Tsujimori T, Zhang R, Liou J G.2007. Permo-Triassic collision, subduction-zonemetamorphism, and tectonic exhumation along the east Asian continental margin.Annual Review of Earth and Planetary Sciences,35:73-110
Fedo C M, Sircombe K N, Rainbird R H.2003. Detrital Zircon Analysis of the SedimentaryRecord. Reviews in Mineralogy and Geochemistry,53(1):277-303
Grant M L, Wilde S A, Wu F, Yang J.2009. The application of zircon cathodoluminescenceimaging, Th-U-Pb chemistry and U-Pb ages in interpreting discrete magmatic andhigh-grade metamorphic events in the North China Craton at the Archean/Proterozoicboundary. Chemical Geology,261(1-2):155-171
Halle T G.1927. Palaeozoic plants from central Shansi. Peking: Geological survey of China.1-316
Halle T G.1935. On the distribution of the Late Palaeozoic floras in Asia. Geografiska Annaler,17:106-111
Jia D, Hu R, Lu Y, Qiu X.2004. Collision belt between the Khanka block and the North Chinablock in the Yanbian Region, Northeast China. Journal of Asian Earth Sciences,23(2):211-219
Jian P, Kr ner A, Windley B F, Shi Y, Zhang W, Zhang L, Yang W.2012. Carboniferous andCretaceous mafic–ultramafic massifs in Inner Mongolia (China): A SHRIMP zircon andgeochemical study of the previously presumed integral―Hegenshan ophiolite‖. Lithos,142–143(0):48-66
Kawasaki S.1927. The Flora of the Heian System, Pt.1. Bull. Geol. Surv. of Chosen,6(1-2):1-30, pls.31-99
Kawasaki S.1934. The Flora of the Heian System, Pt.2. Bull. Geol. Surv. of Chosen,6(4):47-311, pls.105-110
Kawasaki S, Konno E.1932. The Flora of the Heian System, Pt.3. Bull. Geol. Surv. of Chosen,6(3):31-44,61-279, pls.100-104
Khain E V, Bibikova E V, Kr ner A, Zhuravlev D Z, Sklyarov E V, Fedotova A A,Kravchenko-Berezhnoy I R.2002. The most ancient ophiolite of the Central Asian foldbelt: U-Pb and Pb-Pb zircon ages for the Dunzhugur Complex, Eastern Sayan, Siberia,and geodynamic implications. Earth and Planetary Science Letters,199(3-4):311-325
Khain E V, Bibikova E V, Salnikova E B, Kr ner A, Gibsher A S, Didenko A N, Degtyarev K E,Fedotova A A.2003. The Palaeo-Asian ocean in the Neoproterozoic and earlyPalaeozoic: new geochronologic data and palaeotectonic reconstructions. PrecambrianResearch,122(1-4):329-358
Kon'no E.1960. Schizoneura manchuriensis Kon'no and its Fructification (Manchurostachys n.gen.) from the Gigantopteris-nicotianaefolia-bearing Formation in Penchihu Coal-field,Northeastern China. Science Reports, Tohoku University, Sendai, Japan, Spec. Vol.(4):163-188
Kon'no E.1968. The Upper Permian Flora from the Eastern Border of Northeast China. ScienceReports of the Tohoku University, second series (Geology),39(3):159-211, pls.111-125
Koschek G.1993. Origin and significance of the SEM cathodoluminescence from zircon. Journalof Microscopy,171(3):223-232
Kotlyar G V, Belyansky G C, Burago V I, Nikitina A P, Zakharov Y D, Zhuravlev A V.2006.South Primorye, Far East Russia—A key region for global Permian correlation. Journalof Asian Earth Sciences,26(3-4):280-293
Lee D.1987. Geology of Korea. Seoul: The Kyohak-sa Publishing Co.1-514
Li D, Chen Y, Wang Z, Hou K, Liu C.2011a. Detrital zircon U-Pb ages, Hf isotopes and tectonicimplications for Palaeozoic sedimentary rocks from the Xing-Meng orogenic belt,middle-east part of inner Mongolia, China. Geological Journal,46(1):63-81
Li H, Xu Y, Huang X, He B, Luo Z, Yan B.2009. Activation of northern margin of the NorthChina Craton in Late Paleozoic: Evidence from U-Pb dating and Hf isotopes of detritalzircons from the Upper Carboniferous Taiyuan Formation in the Ningwu-Jingle basin.Chinese Science Bulletin,54(4):677-686
Li J Y.2006. Permian geodynamic setting of Northeast China and adjacent regions: closure ofthe Paleo-Asian Ocean and subduction of the Paleo-Pacific Plate Journal of Asian EarthSciences,26(3-4):207-224
Li S Z, Zhao G C, Santosh M, Liu X, Dai L M.2011b. Palaeoproterozoic tectonothermalevolution and deep crustal processes in the Jiao-Liao-Ji Belt, North China Craton: areview. Geological Journal,46(6):525-543. doi:10.1002/gj.1282
Li W, Zhong R, Xu C, Song B, Qu W.2012. U–Pb and Re–Os geochronology of the BainaimiaoCu–Mo–Au deposit, on the northern margin of the North China Craton, Central AsiaOrogenic Belt: Implications for ore genesis and geodynamic setting. Ore GeologyReviews, In press. doi:10.1016/j.oregeorev.2012.03.001
Li X, Wu X.1996. Late paleozoic phytogeographic provinces in China and its adjacent regions.Review of Palaeobotany and Palynology,90(1-2):41-62
Liu L J, Wang X F, Yao Z Q.1996. Emplectopteris and allied pteridosperms from the KaipingBasin, China. Palaeontographica Abt B,239:109-136
Lu X-P, Wu F-Y, Guo J-H, Wilde S A, Yang J-H, Liu X-M, Zhang X-O.2006. Zircon U-Pbgeochronological constraints on the Paleoproterozoic crustal evolution of the Easternblock in the North China Craton. Precambrian Research,146(3-4):138-164
Luo Y, Sun M, Zhao G, Li S, Xu P, Ye K, Xia X.2004. LA-ICP-MS U-Pb zircon ages of theLiaohe Group in the Eastern Block of the North China Craton: constraints on theevolution of the Jiao-Liao-Ji Belt. Precambrian Research,134(3-4):349-371
Markevich P V, Zakharov Y D.2008. Triassic and Jurassic of the Sikhote-Alin:Volcano-Sedimentary assemblage, Paleobiogeography (in Russian). Vladivostok:Dalnauka.1-299
McElhinny M W, Embleton B J J, Ma X H, Zhang Z K.1981. Fragmentation of Asia in thePermian. Nature,293(5829):212-216
Mei M, Huang Q C, Du M, Dilcher D L.1996. The Xu-Huai-Yu Subprovince of the CathaysianFloral Province. Review of Palaeobotany and Palynology,90(1-2):63-77
Meng E, Xu W-L, Pei F-P, Yang D-B, Yu Y, Zhang X-Z.2010. Detrital-zircon geochronology ofLate Paleozoic sedimentary rocks in eastern Heilongjiang Province, NE China:Implications for the tectonic evolution of the eastern segment of the Central AsianOrogenic Belt. Tectonophysics,485(1-4):42-51
Naugolnykh S V.2002. Paracalamitina striata--a Newly Reconstructed Equisetophyte from thePermian of Angaraland. Journal of Paleontology,76(2):377-385
Seyfullah L J, Hilton J.2009. Re-evaluation of Halle's fertile pteridosperms from the Permianfloras of Shanxi Province, China. Plant Systematics and Evolution,279(1-4):191-218
Seyfullah L J, Hilton J.2011. Callistophytalean pteridosperms from Permian aged floras ofChina. Palaeontology,54(2):287-302
Shen S-Z, Zhang H, Shang Q H, Li W-Z.2006. Permian stratigraphy and correlation ofNortheast China: A review. Journal of Asian Earth Sciences,26(3-4):304-326
Shi G R.2006. The marine Permian of East and Northeast Asia: an overview of biostratigraphy,palaeobiogeography and palaeogeographical implications. Journal of Asian EarthSciences,26(3-4):175-206
Stockmans F, Mathieu F-F.1939. La Flore Paleozoique du Bassin Houiller de Kaiping (Chine).Bruxelles.49-165, pls.161-134
Stockmans F, Mathieu F-F.1957. La Flore Paleozoique du Bassin Houiller de Kaiping(Chine)(Deuxieme Partie). Bruxelles.1-89, pls.81-15
Sun K-Q.2006. The Cathaysia Flora and the Mixed Late Permian Cathaysian-Angaran Floras inEast Asia. Journal of Integrative Plant Biology,48(4):381-389
Wang C-w, Sun Y-w, Li N, Zhao G-w, Ma X-q.2009. Tectonic implications of Late Paleozoicstratigraphic distribution in Northeast China and adjacent region. Science in ChinaSeries D-Earth Sciences,52(5):619-626
Wang C, Li N, Sun Y, Zong P.2011. Distribution of Tuvaella Brachiopod Fauna and its tectonicSignificance. Journal of Earth Science,22(1):11-19
Wang J.2010. Late Paleozoic macrofloral assemblages from Weibei Coalfield, with reference tovegetational change through the Late Paleozoic Ice-age in the North China Block.International Journal of Coal Geology,83(2-3):292-317
Wang J, Pfefferkorn H W, Zhang Y, Feng Z.2012. Permian vegetational Pompeii from InnerMongolia and its implications for landscape paleoecology and paleobiogeography ofCathaysia. Proceedings of the National Academy of Sciences,109(13):4927-4932. doi:10.1073/pnas.1115076109
Wilde S A, Valley J W, Peck W H, Graham C M.2001. Evidence from detrital zircons for theexistence of continental crust and oceans on the Earth4.4Gyr ago. Nature,409(6817):175-178
Wilde S A, Wu F-Y, Zhao G.2010. The Khanka Block, NE China, and its significance for theevolution of the Central Asian Orogenic Belt and continental accretion. GeologicalSociety, London, Special Publications,338:117-137
Wu F-Y, Sun D-Y, Ge W-C, Zhang Y-B, Grant M L, Wilde S A, Jahn B-M.2011. Geochronologyof the Phanerozoic granitoids in northeastern China. Journal of Asian Earth Sciences,41(1):1-30
Wu F-Y, Yang J-H, Lo C-H, Wilde S A, Sun D-Y, Jahn B-M.2007a. The Heilongjiang Group: AJurassic accretionary complex in the Jiamusi Massif at the western Pacific margin ofnortheastern China. Island Arc,16(1):156-172
Wu F-Y, Yang J-H, Wilde S A, Liu X-M, Guo J-H, Zhai M-G.2007b. Detrital zircon U-Pb andHf isotopic constraints on the crustal evolution of North Korea. Precambrian Research,159(3-4):155-177
Wu F-Y, Zhao G-C, Sun D-Y, Wilde S A, Yang J-H.2007c. The Hulan Group: Its role in theevolution of the Central Asian Orogenic Belt of NE China. Journal of Asian EarthSciences,30(3-4):542-556
Xiao W J, Windley B F, Hao J, Zhai M G.2003. Accretion leading to collision and the PermianSolonker suture, Inner Mongolia, China: Termination of the central Asian orogenic belt.Tectonics,22(6),1069. doi:10.1029/2002TC001484
Xu X, Harbert W, Dril S, Kravchinksy V.1997. New paleomagnetic data from theMongol-Okhotsk collision zone, Chita region, south-central Russia: implications forPaleozoic paleogeography of the Mongol-Okhotsk ocean. Tectonophysics,269(1-2):113-129
Yang J-H, Wu F-Y, Shao J-A, Wilde S A, Xie L-W, Liu X-M.2006. Constraints on the timing ofuplift of the Yanshan Fold and Thrust Belt, North China. Earth and Planetary ScienceLetters,246(3-4):336-352
Zhang S H, Zhao Y, Song B, Yang Z Y, Hu J M, Wu H.2007. Carboniferous granitic plutonsfrom the northern margin of the North China block: implications for a late Palaeozoicactive continental margin. Journal of the Geological Society,164(2):451-463
Zhang Y, Wu F, Wilde S A, Zhai M, Lu X, Sun D.2004. Zircon U-Pb ages and tectonicimplications of 'Early paleozoic' granitoids at Yanbian, Jilin Province, northeast china.Island Arc,13(4):484-505
Zhang Y, Wu F, Zhai M, Lu X.2005. Tectonic setting of the Helong Block: Implications for thenorthern boundary of the eastern North China Craton. Science in China Ser. D EarthSciences,48(10):1599-1612
Zhao G, Sun M, Wilde S A, Sanzhong L.2005. Late Archean to Paleoproterozoic evolution ofthe North China Craton: key issues revisited. Precambrian Research,136(2):177-202
Zhao G, Wilde S A, Cawood P A, Sun M.2001. Archean blocks and their boundaries in the NorthChina Craton: lithological, geochemical, structural and P-T path constraints and tectonicevolution. Precambrian Research,107(1-2):45-73
Zhao X, Coe R S.1987. Paleomagnetic constraints on the collision and rotation of North andSouth China. Nature,327(6118):141-144
Zhao X, Coe R S, Yaoxiu Z, Haoruo W, Jie W.1990. New paleomagnetic results from northernChina: collision and suturing with Siberia and Kazakhstan. Tectonophysics,181(1-4):43-81
Zhou J-B, Wilde S A, Zhang X-Z, Zhao G-C, Liu F-L, Qiao D-W, Ren S-M, Liu J-H.2011. A>1300km late Pan-African metamorphic belt in NE China: New evidence from theXing'an block and its tectonic implications. Tectonophysics,509(3-4):280-292
Zhou J-B, Wilde S A, Zhang X-Z, Zhao G-C, Zheng C-Q, Wang Y-J, Zhang X-H.2009. Theonset of Pacific margin accretion in NE China: Evidence from the Heilongjianghigh-pressure metamorphic belt. Tectonophysics,478(3-4):230-246
Boucot A J,陈旭, Scotese C R,樊隽轩.2009.显生宙全球古气候重建.北京:科学出版社.1-173
陈旭,阮亦萍,布科AJ.2001.中国古生代气候演变.北京:科学出版社.1-325
窦亚伟,孙喆华,吴绍祖,顾道源.1983.西北地区古生物图册新疆维吾尔自治区分册（二）（晚古生代）.北京:地质出版社.561-614
耿元生,沈其韩,任留东.2010.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,26(7):1945-1966
郭孟习,孙炜,尹国义,彭玉鲸.2000.郯庐断裂系的北延及地质-地球物理特征.吉林地质,19(3):35-44
郭胜哲,苏养正,池永一,黄本宏.1992.吉林、黑龙江东部地槽区古生代生物地层及岩相古地理.见:南润善,郭胜哲编.内蒙古-东北地槽区古生代生物地层及古地理.北京:地质出版社.71-146
郭晓丹,周建波,张兴洲,邱海峻.2011.内蒙古西乌珠穆沁旗本巴图组碎屑锆石LA-ICP-MS U-Pb年龄及其意义.地质通报,30(Z1):278-290
Gu et Zhi.1974.中国植物化石：第一册，中国古生代植物.北京:科学出版社.1-277
韩江,聂立军.2003.吉林省延边开山屯地区大蒜沟组生物化石的发现及其意义.吉林地质,22(3):19-23
韩杰,周建波,张兴洲,邱海峻.2011.内蒙古林西地区上二叠统林西组砂岩碎屑锆石的年龄及其大地构造意义.地质通报,30(Z1):258-269
何锡麟,梁敦士,沈树忠.1996.中国江西二叠纪植物群研究.徐州:中国矿业大学出版社.1-300
何锡麟,朱梅丽,范炳恒,庄寿强,丁惠,薛庆远.1995.山西太原东山晚古生代地层划分对比及古生物研究.长春:吉林大学出版社.1-149, pls.141-172
黑龙江地质矿产局.1993.黑龙江省区域地质志.北京:地质出版社:1-734
黄本宏.1976.华北地区古生物图册内蒙古分册（一）古生代部分.北京:地质出版社.355-379
黄本宏.1977.小兴安岭东南部二叠纪植物群.北京:地质出版社.1-79
黄本宏.1980.古植物.见:沈阳地质矿产研究所编.东北地区古生物图册（一）古生代分册.北京:地质出版社.522-573
黄本宏.1982.东北北部石炭二叠纪陆相地层及古地理概况.地质论评,28(5):395-402
黄本宏.1983.天山-兴安褶皱区东部古生代末植物地理区系及其地质意义.见:唐克东编.中国北方板块构造文集(第一集).138-155
黄本宏.1986a.华夏植物群特有植物——织羊齿(Emplectopteris).中国地质科学院沈阳地质矿产研究所所刊,(14):137-145
黄本宏.1986b.内蒙古镶黄旗地区早二叠世植物化石.见:唐克东编.中国北方板块构造论文集.北京:地质出版社:115-135
黄本宏.1987.辽宁省东部及南部中、晚石炭世地层及植物化石.中国地质科学院沈阳地质矿产研究所所刊,15:43-76
黄本宏.1993.大兴安岭地区石炭、二叠系及植物群.北京:地质出版社.1-141
黄本宏.1995.安加拉植物群在我国石炭纪、二叠纪的分布及其与华夏植物群的关系.见:李星学编.中国地质时期植物群.广州:广东科技出版社.174-189
黄本宏.1997.长白山地晚古生代地层及植物群.中国地质科学院沈阳地质矿产研究所集刊,(5-6):185-268
黄本宏.2000.内蒙古高原晚古生代植物群.植物学通报,17(专辑):172-178
黄汲清,任纪舜,姜春发,张正坤,秦德余.1980.中国大地构造及其演化——1:400万中国大地构造图简要说明.北京:科学出版社.1-124
黄联盟,黄玉宁,梅美堂,李生盛.1989.闽西南早二叠世含煤地层及植物群.北京:煤炭工业出版社.1-101
吉林省地质局第四地质队.1966.1/20万《大兴沟幅》K-52-Ⅳ区域地质测量报告书.长春:吉林省地质局.1-59
吉林省地质局区域地质测量大队.1978.1/20万《敦化县幅》K-52-3区域地质调查报告（地质部分）.长春:吉林省地质局.1-213
吉林省地质局区域地质测量大队第二分队.1965.1/20万《大拉子幅》K-52-ⅩⅥ区域地质测量报告书（地质部分）.长春:吉林省地质局.1-100
吉林省地质局区域地质测量大队第三分队.1965.1/20万《珲春幅》K-52-11，《春化幅》K-52-12区域地质测量报告书.长春:吉林省地质局.1-36
吉林省地质矿产局.1988.吉林省区域地质志.北京:地质出版社.1-698
吉林省区域地层表编写组.1978.东北地区区域地层表吉林省分册.北京:地质出版社.1-214
今野圓蔵.1947.滿洲本溪湖炭田及間島省開山屯附近の二疊系の層序學的並に古植物學的研究.地質學雜誌,53(622-627):102-103
金建华,杜小弟.1993.小兴安岭东南部晚二叠世地层新认识.煤田地质与勘探,21(3):7-12
金玉玕,王向东,尚庆华,王玥,盛金章.1999.中国二叠纪年代地层划分和对比.地质学报,73(2):97-108
寇晓威.1994.吉林省大黑山条垒中部早二叠世地层的发现及其意义.吉林地质,13(1):35-41
郎嘉彬,王成源.2010.吉林磐石地区鹿圈屯组的牙形刺.吉林大学学报(地球科学版),40(3):603-609
李春昱.1980.中国板块构造的轮廓.中国地质科学院院报,2(1):11-22
李春昱,王荃.1983.我国北部边陲及邻区的古板块构造与欧亚大陆的形成.见:唐克东编.中国北方板块构造文集(第一集).3-17
李东津.1997.吉林省岩石地层.武汉:中国地质大学出版社.1-324
李锦轶.1986.内蒙古东部中朝板块与西伯利亚板块之间古缝合带的初步研究.科学通报,(14):1093-1096
李明松,孙跃武,葛文春,张彦龙.2011a.吉林延边地区开山屯植物群的时代——碎屑锆石U-Pb年代学约束编.中国古生物学会第26届学术年会论文摘要集.贵州关岭.99-100
李明松,孙跃武,赵国伟.2011b.吉林延边地区汪清县大兴沟早二叠世华夏植物群的发现及其地质意义.地球科学进展,26(3):339-346
李双林,欧阳自远.1998.兴蒙造山带及邻区的构造格局与构造演化.海洋地质与第四纪地质,18(3):45-54
李星学.1963.华北月门沟群植物化石.北京:科学出版社.1-185
李星学.1980.东亚华夏植物群的鳞木类植物.中国科学,(2):166-171
李星学.1995.中国地质时期植物群.广州:广东科技出版社.1-542
李星学,沈光隆,田宝霖,王士俊,欧阳舒.1995.我国石炭纪、二叠纪植物群的几个论题.见:李星学编.中国地质时期植物群.广州:广东科技出版社.190-226
李星学,姚兆奇.1983.东亚石炭纪和二叠纪植物地理分区.见:古生物学基础理论丛书编委会编.中国古生物地理区系.北京:科学出版社.74-82
李忠,彭守涛,许承武,韩银学,翟明国.2009.韩国太白山盆地古生界砂岩碎屑锆石U-Pb年代及其区域构造含义.岩石学报,25(1):182-192
刘爱,张川波,文琼英.1994.吉林省“槽区”二叠系岩相古地理再造:未出版.1-144
刘爱，赵成弼.1998.延边石炭二叠系一个新的重要植物化石层位的发现.吉林地质:82
刘洪筹,沈光隆.1978.甘肃龙首山石炭纪和二叠纪植物群.兰州:兰州大学.1-152,pls.151-148
马醒华,邢历生,杨振宇,徐树金,张景鑫.1993.鄂尔多斯盆地晚古生代以来古地磁研究.地球物理学报,36(1):68-79
马醒华,杨振宇.1993.中国三大地块的碰撞拼合与古欧亚大陆的重建.地球物理学报,36(4):476-488
梅因C B,姚兆奇编译.1991.欧亚大陆古生代植物群和植物地理学.南京:南京大学出版社.1-177
米家榕,刘茂强.1985.吉林桦甸早二叠世大河深组的心脉羊齿(Cardioneura)古生物学报,24(6):618-624
彭玉鲸.1996.吉林省石炭-二叠纪生物地理区的划分.吉林地质,15(1):12-18
彭玉鲸.1997.解放村植物群的特征及其大地构造意义.吉林地质科技情报,(1):2-8
彭玉鲸,陈跃军,殷长建,李睿.2005.吉黑造山带古生代地层与混杂岩.世界地质,24(1):24-29
彭玉鲸,刘爱,李文国,赵成弼.1999.吉林省延边地区二叠纪的三类植物群与古陆缘再造.吉林地质,18(1):1-23
任纪舜,陈廷愚,牛宝贵,刘志刚,刘凤仁.1990.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.1-205
任纪舜,王作勋,陈炳蔚,姜春发,牛宝贵,李锦轶,谢广连,和政军,刘志刚.1999.从全球看中国大地构造：中国及邻区大地构造图简要说明.北京:地质出版社.1-50
邵济安,唐克东.1995.吉林省延边开山屯地区蛇绿混杂岩.岩石学报,11(增刊):212-220
邵济安,唐克东,詹立培,李子舜,徐公愉,王成源.1995.一个古大陆边缘的再造及其大地构造意义——延边地质研究新进展.中国科学(B辑化学生命科学地学),25(5):548-555
沈光隆.1995.二叠纪植物群.见:李星学编.中国地质时期植物群.广州:广东科技出版社.94-173
石新增.1985.吉林省二叠纪植物地理分区的点滴认识.吉林地质,4(2):47-52
斯行健.1989.内蒙古清水河及山西河曲晚古生代植物群.北京:科学出版社.1-268
宋彪,张玉海,万渝生,简平.2002.锆石SHRIMP样品靶制作、年龄测定及有关现象讨论.地质论评,48(增刊):26-30
孙柏年,沈光隆,刘燕学.1993.新疆塔里木盆地北缘的陆相下二叠统.兰州大学学报,29(1):110-115
孙德有,吴福元,张艳斌,高山.2004.西拉木伦河-长春-延吉板块缝合带的最后闭合时间———来自吉林大玉山花岗岩体的证据.吉林大学学报(地球科学版),34(2):174-181
孙革.1991.山西保德早二叠世Cordaites baodeensis sp. nov.叶表皮构造及Cordaites分类探讨.古生物学报,30(2):167-185
孙革.1993.中国吉林天桥岭晚三叠世植物群.长春:吉林科学技术出版社.1-157
孙革,赵衍华.1992.古生代植物.见:吉林省地质矿产局编.吉林省古生物图册.长春:吉林科技出版社.504-562
孙恒元.1984.吉林省延边地区晚石炭世的蜓类化石带.吉林地质,3(3):38-44
孙恒元.1988.吉林延边地区二叠系研究的进展.地层学杂志,12(3):202-229
孙恒元.1990.吉林延边地区二叠系大蒜沟组蜓类化石.微体古生物学报,7(3):257-264
孙克勤.1992.山东淄博地区晚石炭世和早二叠世植物群、古生态及沉积环境.长春:吉林大学出版社.1-143
孙克勤,邓胜徽.2003.贺兰山北段石炭纪和二叠纪植物群.现代地质,(03):259-267,357-358
孙克勤,张周良,阴家润,胡善亭.1996.贺兰山北段晚石炭世和早二叠世植物群古生态研究.现代地质,10(3):25-33
孙晓猛,王书琴,王英德,杜继宇,许强伟.2010.郯庐断裂带北段构造特征及构造演化序列.岩石学报,26(1):165-176
孙跃武,李明松,赵国伟.2012.吉林延边地区早二叠世一个新的陆相地层单位.地层学杂志,36(1):89-96
唐克东.1989.中朝陆台北侧褶皱带构造发展的几个问题.现代地质,3(2):195-204
唐克东,邵济安,李景春,康庄.2004.吉林延边缝合带的性质与东北亚构造.地质通报,23(9-10):885-891
唐克东,赵爱林.2007.吉林延边开山屯地区地层时代的新证据.地层学杂志,31(2):141-150
万天丰.2004.中国大地构造学纲要.北京:地质出版社.1-387
万天丰,朱鸿.1996.郯庐断裂带的最大左行走滑断距及其形成时期.高校地质学报,2(1):14-27
万天丰,朱鸿,赵磊,林建平,程捷,陈进.1996.郯庐断裂带的形成与演化：综述.现代地质,10(2):159-168
王成文,金巍,张兴洲,马志红,迟效国,刘永江,李宁.2008.东北及邻区晚古生代大地构造属性新认识.地层学杂志,32(2):119-136
王成文,孙跃武,李宁,刘欢,赵国伟.2009.东北地区晚古生代地层分布规律.地层学杂志,33(1):56-61
王鸿祯.1981.从活动论观点论中国大地构造分区.地球科学,(1):42-66
王鸿祯.1982.中国地壳构造发展的主要阶段.地球科学,18(3):155-178
王鸿祯.1985.中国古地理图集.北京:地图出版社.1-143
王鸿祯,刘本培.1981.中国中元古代以来古地理发展的轮廓.地层学杂志,5(2):77-89
王小凤,李中坚,陈柏林,陈宣华,董树文,张青,武红岭,邢历生,张宏,董法先,邬华梅,霍光辉,林传勇,白嘉启,刘晓春.2000.郯庐断裂带.北京:地质出版社.1-374
王玉净,樊志勇.1997.内蒙古西拉木伦河北部蛇绿岩带中二叠纪放射虫的发现及其地质意义.古生物学报,36(1):58-69
王钰,卢衍豪,杨敬之,穆恩之,盛金章.1954.辽东太子河流域地层(Ⅱ).地质学报,34(2):89-145
吴秀元,孙柏年,沈光隆,王永栋.1997.塔里木盆地北缘二叠纪植物群.古生物学报,36(S1):3-26
徐嘉炜.1980.郯—庐断裂带巨大的左行平移运动.合肥工业大学学报,(1):1-26+127-128
徐嘉炜.1985.郯庐断裂带北段平移研究的若干进展——答乔秀夫的“对郯庐断裂巨大平移质疑”.地质论评,31(1):83-86
徐嘉炜,崔可锐,刘庆,童蔚欣,朱光.1985.东亚大陆边缘中生代的左行平移断裂作用.海洋地质与第四纪地质,5(2):51-64
徐嘉炜,马国锋.1992.郯庐断裂带研究的十年回顾.地质论评,38(4):316-324
徐永文,贾连镇.1983.1/20万《珲春县幅》K-52-11，《春化幅》K-52-12，《敬信公社幅》K-52-17区域地质调查报告(地质部分).长春:吉林省地质矿产局区域地质调查大队.1-272
徐永文,殷长建.1991.1/5万《后河幅》K-52-19-D，《大兴沟镇幅》K-52-20-C区域地质调查报告：地质部分.长春:吉林省地质矿产局区域地质矿产调查所.1-186
阎同生,杨遵仪.2001.河北抚宁、曲阳晚古生代地层及植物群.北京:地质出版社.1-89
杨关秀,陈钟惠,张守良.1983.内蒙古准格尔旗东部太原组、山西组植物群特征.地球科学,(4):69-83,168-171
杨关秀等.2006.中国豫西二叠纪华夏植物群——禹州植物群.北京:地质出版社.1-361
杨涛.2010.吉林珲春晚二叠世解放村植物群.吉林大学,博士:1-101
叶茂,张世红,吴福元.1994.中国满洲里－绥芬河地学断面域古生代构造单元及其地质演化.长春地质学院学报,24(3):241-245
殷长建,孙春林,彭玉鲸,周晓东,赵衍华.2003.敦化隆起东缘晚石炭—早二叠世华夏植物群的发现及其地质意义.吉林大学学报(地球科学版),33(3):257-262
昝淑芹,高嘉瑞.1994.敦化-密山断裂带的特征、演化及与郯-庐断裂的关系.北京:地震出版社.52-57
张泓.1988.安加拉古陆外围晚二叠世混生植物群特征及形成机制的讨论.地质论评,34(4):343-350
张炯飞.1997.延边地区渤海地块与兴凯地块之间古缝合带的初步研究.吉林地质,16(2):30-37
张炯飞,张允平.1995.关于延边地区石炭-二叠系.中国地质科学院沈阳地质矿产研究所集刊,4:1-7
张开均.1998.华北板块东缘晚古生代火山活动及其大地构造含义.中国煤田地质,10(3):10-11,20
张理刚.1992.中国东部岩石圈铅同位素化学结构与动力学研究.矿物岩石地球化学通讯,11(3):133-137
张梅生,彭向东,孙晓猛.1998.中国东北区古生代构造古地理格局.辽宁地质,(2):12-17
张善桢,孙革,赵衍华.1987.吉林磐石吉昌地区早石炭世植物研究初报.古生物学报,26(4):456-470
张晓晖,翟明国.2010.华北北部古生代大陆地壳增生过程中的岩浆作用与成矿效应.岩石学报,26(5):1329-1341
张兴洲,穆石敏,杨宝俊,迟晓国.1999.拼合的大陆板块.见:张贻侠,孙运生,张兴洲,杨宝俊编.中国满洲里-绥芬河地学断面1：1000000说明书.北京:地质出版社.6-19
张兴洲,周建波,孙跃武,张凤旭,刘永江,朱占平,彭晓蕾,赵庆英,郎嘉彬,张淑芹,温泉波,迟效国,葛文春.2012.松辽盆地及外围上古生界石油地质综合研究2011年度中期工作报告.长春:吉林大学.
张宜.2009.山西保德晚古生代植物群.中国科学院南京地质古生物研究所,博士:1-157
张永焕,彭玉鲸,欧祥喜.2000.关于吉林省延边地区二叠纪地层的思考.吉林地质,19(1):1-12
赵春荆,彭玉鲸,党增欣,等.1996.吉黑东部构造格架及地壳演化.沈阳:辽宁大学出版社.1-186
赵修祜,刘陆军,侯吉辉.1987.晋东南地区晚古生代含煤地层和古生物群.南京:南京大学出版社.61-137
赵修祜,莫壮观,张善桢,姚兆奇.1980.黔西滇东晚二叠世植物群编.黔西滇东晚二叠世含煤地层和古生物群.北京:科学出版社.70-122
赵英利,刘永江,韩国卿,温泉波,李伟,梁道俊.2009.敦-密断裂左行走滑三维有限元模拟.世界地质,28(3):310-317
針尾慶次,川越浩.1923.間島豆滿江沿岸地質調查報告.南滿洲鐵道株式會社地質調查所.1-23
中国地质科学院地质研究所,新疆地矿局地质科学研究所.1986.新疆吉木萨尔大龙口二叠三叠纪地层及古生物群.北京:地质出版社.1-262
周晓东.2009.吉林省中东部地区下石炭统—下三叠统地层序列及构造演化.吉林大学,博士:1-103
周晓东,殷长建,彭玉鲸.2009.吉林延边地区柯岛群之由来及再认识.世界地质,28(1):37-44
朱光,宋传中,王道轩,刘国生,徐嘉炜.2001.郯庐断裂带走滑时代的40Ar/39Ar年代学研究及其构造意义.中国科学（D辑）,31(3):250-256
朱彤.1990.福建二叠纪含煤地层及古生物群.北京:地质出版社.1-127
© 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 |