中国南方古生界海相烃源岩的主变形期

doi:10.11743/ogg20080506

摘要/Abstract

摘要：

中国南方海相碳酸盐岩层系中发育了多套烃源岩,它们在沉积之后经历了多期构造事件。在野外观测和地震剖面解释的基础上,对中国南方海相烃源岩的变形序列进行了剖析,甄别出4个变形期,分别为早古生代晚期(421～441 Ma)、晚三叠世(215～230 Ma)、晚侏罗世—早白垩世和早白垩世—第三纪,并指出中生代中晚期为主变形期,形成了不同尺度的叠加构造。

关键词: 叠加构造, 主变形期, 海相烃源岩, 中生代, 中国南方

Abstract:

There are multiple sets of hydrocarbon source rocks developed in South China,which experienced several tectonic events.By analyzing deformation succession,four deformation phases are recognized for Paleozoic marine hydrocarbon source rocks in South China,on a basis of field observation and seismic section interpretation,i.e.,late Early Paleozoic(421-441 Ma),Late Triassic(215-230 Ma),Late Jurassic-Early Cretaceous and Early Cretaceous-Tertiary.It is suggested that the main deformation phases occur in the Middle-Late Mesozoic,forming superimposed structures with different sizes.

Key words: superposed structure, main deformation phase, marine hydrocarbon source rock, Mesozoic, South China

中图分类号:

TE121.1

王清晨,林伟. 中国南方古生界海相烃源岩的主变形期[J]. 石油与天然气地质, 2008, 29(5): 582-588,622. doi: 10.11743/ogg20080506 Wang Qingchen,Lin Wei. Main deformation phases of the Paleozoic marine hydrocarbon source rocks in South China[J]. Oil & Gas Geology, 2008, 29(5): 582-588,622. doi: 10.11743/ogg20080506

参考文献

[1] 刘光鼎.试论残留盆地.勘探家(石油与天然气),1997,2(3):1～4
[2] 王清晨,蔡立国.中国南方显生宙大地构造演化简史[J].地质学报,2007,81(8):1025～1040
[3] Li Z X,Kinny P D,Wang J.The breakup of Rodinia:did it start with a mantle plume beneath South China?[J].Earth and Planetary Science Letters,1999,173:171-181
[4] Li Z X,Li X,Zhou H,et al.Grenvillian continental collision in south China:new SHRIMP U-Pb zircon results and implications for the configuration of Rodinia[J].Geology,2002,30:163-166
[5] Ling W,Gan S,Zhang B,et al.Neoproterozoic tectonic evolution of the northwestern Yangtze craton,South China:implications for amalgamation and break-up of Rodinia Supercontinent[J].Precambrian Research,2003,122:111-140
[6] Wang J,Li Z.History of Neoproterozoic rift basins in South China:implications for Rodinia break-up[J].Precambrian Research,2003,122:141-158
[7] 李献华.祁昌实,刘颖,等.扬子块体西缘新元古代双峰式火山岩成因:Hf同位素和Fe/Mn新制约[J].科学通报,2005,50(19):2155～2160
[8] Hsu K J,Sun S,Li J L.Huanan Alps,not South China platform[J].Sci China(Ser B),1988,19(1):110-119
[9] 水涛.中国东南大陆基底构造格局[J].中国科学(B辑),1987,(4):78～86
[10] Chen J,Foland K A Xing F M,et al.Magmatism along the southeast margin of the Yangtze block:Precambrian collision of the Yangtze and Cathaysia blocks of China[J].Geology,1991,19:815-818
[11] Zhou X M,Zhu Y H.Late Proterozoic collisional orogen and gensuture in southeastern China:petrological evidence[J].1993,12:239-251
[12] Li Z X,Zhang L,Powell C McA.South China in Rodinia:part of the missing link between Australia-East Antarctica and Laurentia?[J].Geology,1995,23:407-410
[13] Li X,Li Z X,Ge W,et al.Neoproterozoic granitoids in South China:crustal melting above a mantle plume at CA 825-Ma?[J].Precambrian Research,2003,122:45-83
[14] Huang T K.An outline of the tectonic characteristics of China[J].Ecolgae Geologicae Helvctiae,1978,71:611-635
[15] Ren J.On the Geotectonics of Southern China[J].Acta Geologica Sinica,1991,4:111-127
[16] 刘宝珺,许效松,潘杏南,等.中国南方古大陆沉积地壳演化与成矿[M].北京:科学出版社,1993.1～236
[17] 马力,陈焕疆,甘克文,等.中国南方大地构造和海相油气地质[M].北京:地质出版社,2004.1～867
[18] Yang Z,Sun Z,Yang T,et al.A long connection(750-380 Ms) between South China and Australia:paleomngnetic constraints[J].Earth and Planetary Science Letters,2004,220:423-434
[19] Chung S L,Jahn B M.Plume-lithosphere interaction in generation of the Emeishan flood basalts at the Permian-Triassic boundary[J].Geology,1995,23:889-892
[20] He B,Xu Y,Chung S L,et al.Sedimentary evidence for a rapid,kilometer-scale crustal doming prior to the eruption of the Emeishan flood basalts[J].Earth Planet Sci Lett,2003,213:391-405
[21] 罗志立.中国西南地区晚古生代以来地裂运动对石油等矿产形成的影响[J].四川地质学报,1981,20(2):1～22
[22] 罗志立.略论地裂运动与中国油气分布[J].中国地质科学院院报,1984,21(10):93～101
[23] 罗志立,金以钟,朱夔玉,等.试论上扬子地台的峨眉地裂运动[J].地质论评,1988,34(1):11～23
[24] Wang Q,Li J W,Jian P,et al.Alkaline syenites in eastern Cathaysia(South China):link to Permian-Triassic transtension[J].Earth Planet Sci Lett,2005,230:339-354
[25] Li X,Li Z X,Li W,et al.Initiation of the Indosinian orogeny in South China:evidence for a Permian magmatic arc on Hainan Island[J].The Janrnal of Geology,2006,114:341-353
[26] Wang Y,Zhang Y,Fan W,et al.Structural signatures and 40Ar/39Ar geochronology of the Indosinian Xuefengshan tectonic belt,South China Block[J].Journal of Structural Geology,2005,27:985-998
[27] Wang D,Shu L,Faure M,et al.Mesozoic magmatism and granitic dome in the Wugongshan Massif,Jiangzi province and their genctical relationship to the tectonic events in southeast China[J].Tectonophysics,2001,339:259-277
[28] Hsu K J,Wang Q,Sun S,et al.Tectonic evolution of Qinling Mountains,China[J].Ecolgoc Geologicae Helvetiae,1987,80:735-752
[29] Sun S,Li J,Lin J,et al.Indesinides in China and the consumption of Eastern paleotethys.In:Muller D W,McKenzie J A,Weissert H,eds.Controversies in modern geology:evolution of geological theories in sodimentaology,earth history and tectonics[M].London:Academic Press,1989.363-384
[30] 张国伟,孟庆任,赖绍聪.秦岭造山带的结构构造[J].中国科学(B辑),1995,25(9):994～1003
[31] 张国伟,张本仁,袁学诚,等.秦岭造山带与大陆动力学[M].北京:科学出版社,2001.1～855
[32] 钟大赉.滇川西部古特提斯造山带[M].北京:科学出版社,1998.1～231
[33] Wang X,Metcalfe I,Ping J,et al.The Jinshajiang-Ailaoshan Suture Zone,China:tectenostratigraphy,age and evolution[J].Journal of Asian Earth Sciences,2000,18:675-690
[34] Metcalfe I.Permain tectonic framework and palaeogeography of SE Asia[J].Journal of Asian Earth Sciences,2002,20:551-566
[35] Li P,Gao R,Cui J,et al.Paleomagmetic analysis of eastern Tibet:implications for the collisional and amalgamation history of the Three Rivers Region,SW China[J].Journal of Asian Earth Sciences,2004,24:291-310
[36] Zhou X M,Li W X.Origin of Late Mesozoic igneous rocks in Southeastern China:implications for lithosphere subduction and underplating of mafic magmas[J].Tectonophysics,2000,326:269-287
[37] Yan D P,Zhou M F,Song H L,et al.Origin and tectonic significance of a Mesozoic muti-layer over-thrust system within the Yangtze bock (South China)[J].Tectonophysics,2003,361:239-254
[38] Tapponnier P,Xu Z,Roger F,et al.,Oblique stepwise rise and growth of the Tibet Plateau[J].Science,2001,294:1671-1677
[39] Teng L S.Geotectonic evolution of Late Cenozoic arc-continent collision in Taiwan[J].Tectonophysics,1990,183:57-76
[40] 广西壮族自治区地质矿产局.广西壮族自治区区域地质志[M].北京:地质出版社,1985.1～853
[41] 尹赞勋,张守信,谢翠华.论褶皱幕[M].北京:科学出版社,1980.1～106
[42] Li X,Tatsumoto P M,et al.Age and origin of the Tanghu granite,southeast China:result from U-Pb single zircon and Nd isotopes[J].Geology,1989,17:395-399
[43] Chen J,Jahn B M.Crustal evolution of southeastern China:Nd and Sr isotopic evidence[J].Tectonophysics,1998,284:101-133
[44] 杨树峰.成对花岗岩带和板块构造[M].北京:科学出版社,1987.1～98