TYPES AND CHARACTERISTICS OF THE CATHAYSIAN BLOCK GROUP

QI Jianghao; GUO Xingwei; WEN Zhenhe; ZHANG Xunhua; FANG Nianqiao

doi:10.3724/SP.J.1140.2014.06027

Marine Geology & Quaternary Geology > 2014 > 34(6): 27-39. > DOI: 10.3724/SP.J.1140.2014.06027

QI Jianghao, GUO Xingwei, WEN Zhenhe, ZHANG Xunhua, FANG Nianqiao. TYPES AND CHARACTERISTICS OF THE CATHAYSIAN BLOCK GROUP[J]. Marine Geology & Quaternary Geology, 2014, 34(6): 27-39. DOI: 10.3724/SP.J.1140.2014.06027

Citation:

PDF (1800 KB)

TYPES AND CHARACTERISTICS OF THE CATHAYSIAN BLOCK GROUP

1. School of Ocean Sciences, China University of Geosciences, Beijing 100083, China;
2. Key Laboratory of Marine Hydrocarbon Resources and Environment Geology, Ministry of Land and Resources, Qingdao Institute of Marine Geology, Qingdao 266071, China

More Information

Received Date: July 19, 2014
Revised Date: October 29, 2014

Graphical Abstract

Abstract

Abstract

The theory of block tectonics was put forward when the mapping project on "Tectonic Frame Map of China and Adjacent Regions" was lunched. With it the crustal evolution of China and adjacent regions is divides into 5 stages:the continental nucleus forming stage, the paleo-global tectonic stage which includes the platform forming stage and the stabilizing stage, the transitional stage and the neo-global tectonic stage. Blocks and junction belts are adopted and redefined as the second order tectonic units under the plate to reveal the tectonic evolution of the paleo-global tectonics stage, as the theory of plate tectonics has successfully illuminated the global tectonic evolution in the neo-global tectonic stage. By Late Permian, there were 3 block groups in China and adjacent regions as part of the Pangea:the Laurasia Block Group, the Cathaysian Block Group and the Gondwana Block Group. The Cathaysian Block Group is composed of a number of smaller blocks which have complicated evolutionary history and rich tectonic information respectively. In this paper, we collected and studied the data of regional tectonics, lithology and stratigraphy, plus detailed analysis of isotope dating data related to tectonic evolution stages, divided the Cathaysian Block Group into three types of North China, Yangtze and South China and stipulated their evolutionary history in detail. The platform forming stage of the North China type was completed in late PaleoProterozoic about 1.8Ga, the platform forming stage of the Yangtze type in early NeoProterozoic about 800 Ma, and the platform forming stage of the South China type by the end of Early Paleozoic 400Ma. Once the platforms were formed, they entered the stabilizing stage until the end of early Permian when they entered the transitional stage. Their evolution shows a similar sequence but different time schedule. After the Indosinian movement, as parts of the Eurasian Plate, the Cathaysian Blocks have moved into the neo-global tectonic stage.
- theory of block tectonics,
- Cathaysian Block Group,
- North China,
- Yangtze,
- South China

FullText(HTML)

References (72)

References

[1]	黄宗理,张良弼. 地球科学大辞典(基础科学卷)[M]. 北京:地质出版社,2006.[HUANG Zongli, ZHANG Liangzhou. Geosciences Dictionary (Basic Sciences)[M]. Beijing:Geological Publishing House,2006.]
[2]	Huang T K.On the major tectonic forms of China[J].Geological Memoirs Ser.A,1945,20:1-165.
[3]	黄汲清,任纪舜,等.1:400万中国大地构造图及说明书"中国大地构造及其演化"[M].北京:科学出版社,1979.[HUANG T K, REN Jishun, et al. Tectonic map of China(1:4000000) and the introduction "Tectonic and evolution of China"[M]. Beijing:Science Press,1979. ]
[4]	李四光.地质力学概论[M].北京:地质出版社,1962.[LI Siguang. Geomechanics Conspectus[M]. Beijing:Geology Press,1962.]
[5]	中国地质科学院地质力学研究所.1:400万中华人民共和国构造体系图及说明书"中国主要构造体系"[M].北京:地图出版社,1985.[Institute of Geomechanics, Chinese Academy of Geological Sciences.Tectonic System Map in People's Republic of China(1:4000000)and the Instruction-"The Main Tectonic Systems in China"[M].Beijing:Cartographical Press,1985. ]
[6]	张文佑.1:400万中国断块构造图及其说明书"中国大地构造基本特征及发展"[M].北京:科学出版社,1974.[ZHANG Wenyou.Fault-Block Tectonic Map in China(1:4000000)and the Instruction-"Basic Characteristics and Development of the Tectonics of China"[M].Beijing:Science Press,1974. ]
[7]	张文佑.断块构造导论[M].北京:石油工业出版社,1984.[ZHANG Wenyou.Introduction to Fault-Block Theory[M].Beijing:Petroleum Industry Publishing House,1984.]
[8]	国家地震局广州地震大队.1:400万中国大地构造图及说明书"中国大地构造概要"[M].北京:地震出版社,1977.[Guangzhou Survey Group of Seismology of State Seismological Bureau.Tectonic map in China(1:4000000) and the Instruction-"Outline of the Tectonics of China"[M].Beijing:Earthquake Publishing House,1977. ]
[9]	陈国达.陈国达地洼学说文选[M].长沙:中南工业大学出版社,1986.[CHEN Guoda.Selected Works of Chen Guoda's Diwa (Geodepression) Theory[M].Changsha:Central South University of Technology Press(in Chinese),1986.]
[10]	张伯声.镶嵌的地壳[J].地质学报,1962,42(3):275-288. [ZHANG Bosheng. The Mosaic Earth Crust[J].Acta Geological Sinica,1962,42(3):275-288.]
[11]	张伯声.1:400万中国镶嵌构造图及说明书"中国地壳的波浪状镶嵌构造"[M].北京:科学出版社,1980.[ZHANG Bosheng.Mosaic Structure Map in China(1:4000000) and the Instruction-"Crustal Wavy Mosaic Structure in China"[M].Beijing:Science Press, 1980. ]
[12]	潘桂棠.中国大地构造单元划分[J].中国地质, 2009,36(1):1-28. [PAN Guitang.Subdivision of tectonic units in China[J].Geology in China,2009,36(1):1-28.]
[13]	Ren J S.The continental tectonics of China[J].Journal of Southeast Asian Earth Science,1996,13(3/5):197-204.
[14]	任纪舜,王作勋,陈炳蔚,等.从全球看中国大地构造-中国及邻域大地构造图及简要说明[M].北京:地质出版社,1999.[REN Jishun, WANG Zuoxun, CHEN Bingwei, et al.The Tectonics of China from a Global View-A Guide to the Tectonic Map of China and Adjacent Regions[M].Beijing:Geological Publishing House, 1999.]
[15]	王鸿祯.中国古地理图集[M].北京:地图出版社,1985.[WANG Hongzhen. Atlas of the Paleogeography of China[M]. Beijing:Cartography Press,1985.]
[16]	WANG Hongzhen, MO Xuanxue.An outline of the tectonic evolution of China[J].Episode,1995,19(5):6-16.
[17]	李春昱.中国板块构造的轮廓[J].中国地质科学院院报,1980,2(1):11-20. [LI Chunyu.A preliminary study of plate tectonics of China[J].Bulletin of Chinese Academy of Geological Science,Series I.,1980,2(1):11-20.]
[18]	李春昱,王荃,刘雪亚,等.亚洲大地构造图(1:800万)[M].北京:地质出版社,1982.[Lee Chunyu, WANG Quan, LIU Xueya, et al.Tectonic map of Asia (1:8000000)[M].Beijing:Geological Publishing House,1982. ]
[19]	刘光鼎. 中国海区及邻域地质地球物理系列图[M]. 北京:科学出版社,1992.[LIU Guangding. Map Series of Geology-Geophysics of China Seas and Adjacent Areas[M]. Beijing:Science Press,1992.]
[20]	张训华,孟祥君,韩波. 块体与块体构造学说[J]. 海洋地质与第四纪地质,2009,19(5):59-64. [ZHANG Xunhua, MENG Xiangjun, HAN Bo. Blocks and block tectonics[J]. Marine Geology and Quaternary Geology,2009,19(5)59-64.]
[21]	刘光鼎,陈洁. 中国前新生代残留盆地油气勘探难点分析及对策[J]. 地球物理学进展, 2005,20(2):273-275. [LIU Guangding, Chen Jie. Analysis of difficulties in gas-petroleum prospecting in Chinese Pre-Cenozoic relic basin and the corresponding solutions[J]. Process in Geophysics, 2005, 20(2):273-275.]
[22]	刘光鼎,郝天珧,刘伊克. 中国大地构造宏观格架及其与矿产资源的关系-根据地球物理资料的认识[J]. 科学通报,1997,42(2):113-118. [LIU Guangding, Hao Tianyao, Liu Yike. China tectonic macro framework-based on the understanding of geophysical data[J].Chinese Science Bulletin,1997,(42)2:113-118.]
[23]	刘光鼎. 中国大陆构造格架的动力学演化[J]. 地学前缘,2007,14(3):39-46. [LIU Guangding. Geodynamical evolution and tectonic framework of China[J]. Earth Science Frontiers,2007,14(3):39-46.]
[24]	Wynne-Edword H R. Proterozoic ensialic orogenesis, the millipede model of ductile plate tectonics[J]. American Journal of Science, 1976, 276:927-953.
[25]	朱夏.试论古全球构造与古生代油气盆地[J]. 石油与天然气地质,1983,4(1):1-33. [ZHU Xia. Notes on ancient global tectonics and Paleozoic petroliferous basins[J]. Oil and Gas Geology,1983,4(1):1-33.]
[26]	朱夏. 关于中国大陆边缘的演化[J]. 海洋地质与第四纪地质,1987,7(3):115-120. [ZHU Xia. On the evolution of continental margins of China[J]. Marine Geology and Quaternary Geology,1987,7(3):115-120.]
[27]	苑凤华,彭玉鲸,周晓东,等. 中国东北兴蒙-吉黑造山带贝加尔运动、萨拉伊尔运动、兴凯运动及泛非运动等之比较[J]. 吉林地质,2012,31(4):2-6. [YUAN Fenghua, PENG Yujing, ZHOU Xiaodong, et al. Comparison of Baikalian orogeny, Salair orogeny, Xingkai orogeny, and Pan-African orogeny of Xingmeng-Jihei orogenesis zone in the Northeast China[J]. Jilin Geology,2012,31(4):2-6.]
[28]	翟明国. 华北克拉通的形成以及早期板块构造[J]. 地质学报,2012,86(9):1335-1347. [ZHAI Mingguo. Evolution of the North China craton and early plate tectonics[J]. Acta Geological Sinica, 2012,86(9):1335-1347.]
[29]	赵宗溥.中朝准地台前寒武纪地壳演化[M]. 北京:科学出版社, 1993:366-388.[ZHAO Zongfu. Sino Korean Paraplat-Form Precambrian Crustal Evolution[M]. Science Press,1993:366 -388.]
[30]	邓晋福,吴宗絮,赵国春,等.华北地台前寒武纪花岗岩类、陆壳演化与克拉通形成[J]. 岩石学报, 1999, 15:190-198.[DENG Jinfu, WU Zongxu, ZHAO Guochun, et al. Precambrian granitic rocks, continental crustal evolution and craton formation of the North China platform[J]. Acta Petrologica Sinica, 1999 , 15:190-198.]
[31]	伍家善,耿元生,沈其韩,等.中朝古大陆太古宙地质特征及构造演化[M]. 北京:地质出版社, 1998:192-211.[WU Jiashan, GENG Yuansheng, SHEN Qihan, et al. Archean Geological and Tectonic Evolution of Sino Korean Ancient Continent[M]. Beijing:Geological Publishing House, 1998:192 -211.]
[32]	Zhai M G, Guo J H, Liu W J. Neoarchean to Paleoproterozoic continental evolution and tectonic history of the North China craton[J]. J. Asian Earth Science, 2005, 24:547-561.
[33]	白瑾,黄学光,戴凤岩,等.中国前寒武纪地壳演化[M]. 北京:地质出版社, 1993:36-38.[BAI Jin, HUANG Xueguang, DAI Fengyan, et al. China Precambrian Crustal Evolution[M]. Beijing:Geological Publishing House, 1993:36 -38.]
[34]	管志宁,安玉林,吴朝均.磁性界面反演及华北地区深部构造的推断[C]//勘查地球物理勘查地球化学文集(第6集).中国区域地球物理研究.北京:地质出版社, 1987:80-101.[GUAN Zhining, AN Yulin, WU Chaojun. Magnetic interface inversion and deep structure inference in North China[C]//Geophysical exploration and geochemistry exploration anthology(Episode 6), China regional geophysical research. Beijing:Geological Publishing House, 1987 :80-101.]
[35]	翟明国.克拉通化与华北陆块的形成[J]. 中国科学:地球科学,2011,41(8):1037-1046. [ZHAI Mingguo. Cratonization and the Ancient North China Continent[J]. A summary and review. Science China Earth Science, 2011, 41(8):1037-1046.]
[36]	Zhai Mingguo. Precambrian Geological Events in the North China Craton[J]. Geol Soc Spe Pub London, 2004, 226:57-72.
[37]	李江海,牛向龙,程素华,等.大陆克拉通早期构造演化历史探讨:以华北为例[J]. 地球科学-中国地质大学学报,2006,31(3):285-292. [LI Jianghai, NIU Xianglong, CHENG Suhua, et al. The Early Precambrian tectonic evolution of continental craton:a case Study from North China[J]. Earth Science -Journal of China University of Geosciences, 2006,31(3):285-292.]
[38]	耿元生,万渝生,沈其韩.华北克拉通早前寒武纪基性火山作用与地壳增生[J]. 地质学报,2002,76(2):199-207. [GENG Yuansheng, WAN Yusheng, SHEN Qihan. Early Precambrian basic volcanism and crustal growth in the North China craton[J]. Acta Geological Sinica, 2002,76(2):199-207.]
[39]	Zhu X Q,Zhu W B,Ge R S, et al. Late Paleozoic provenance shift in the south-central North China Craton:Implications for tectonic evolution and crustal growth[J]. Gondwana Research,2014,24:383-400.
[40]	Geng Y S,Du L L,Ren L D. Growth and reworking of the early Precambrian continental crust in the North China Craton:Constraints from zircon Hf isotopes[J]. Gondwana Research,2012:517-529.
[41]	赵太平,徐勇航,翟明国.华北陆块南部元古宙熊耳群火山岩的成因与构造环境:事实与争议[J]. 高校地质学报,2007,13(2):191-206. [ZHAO Taiping, XU Yonghang, ZHAI Mingguo. Petrogenesis and tectonic setting of the Paleoproterozoic Xiong'er group in the southern part of the North China craton:a review[J]. Geological Journal of China Universities, 2007,13(2):191-206.]
[42]	翟明国.华北克拉通2.1~1.7 Ga地质事件群的分解和构造意义探讨[J]. 岩石学报,2004,20(6):1343-1354. [ZHAI Mingguo. 2.1~1.7 Ga geological event group and its geotectonic significance[J]. Acta Petroligica Sinica, 2004,20(6):1343-1354.]
[43]	翟明国,卞爱国. 华北克拉通新太古代末超大陆拼合及古元古代末-中元古代裂解[J]. 中国科学D辑,2000,30:131-137.[ZHAI Mingguo, BIAN Aiguo. Super continent collision in latest Neoproterozoic and cracking in latest Paleoproterozoic-Mesoproterozoic of the North China Craton[J]. Science in China(Series D),2000 ,30:131-137.]
[44]	高山,QIU Yumin,凌文黎,等.崆岭高级变质地体单颗粒锆石SHRIMP U-Pb年代学研究-扬子克拉通>3.2 Ga陆壳物质的发现[J]. 中国科学D辑,2001,31(1):27-35. [GAO Shan,QIU Yumin, LING Wenli, et al. SHRIMP U-Pb geochronology on Kongling high-grade metamorphic zircon——Discovery of > 3.2 Ga continental crust in the Yangtze craton of south China[J].Science in China(Series D),2001,31(1):27-35.]
[45]	彭敏,吴元保,汪晶,等. 扬子崆岭高级变质地体古元古代基性岩脉的发现及其意义[J]. 科学通报,2009,54(5):641-647. [PENG Min, WU Yuanbao, WANG Jing, et al. Discovery and significance of Kongling high-grade metamorphic Paleoproterozoic mafic dikes in Yangtze[J]. Chinese Science Bulletin, 2009,54(5):641-647.]
[46]	Gao S, Yang J, Zhou L, et al. Age and growth of the Archean Kongling terrain, South China, with emphasis on 3.3 Ga granitoid gneisses[J]. AM.J.Sci.,2011,311:153-182.
[47]	Zhang S B, Zheng Y F, Wu Y B, et al. Zircon isotope evidence for ≥ 3.5 Ga continental crust in the Yangtze cra-ton of China[J]. Precambrian Res., 2006, 146:16-34.
[48]	Zhang S B, Zheng Y F, Wu Y B, et al. Zircon U-Pb age and Hf-O isotope evidence for Paleoproterozoic meta-morphic event in South China[J]. Precambrain Res., 2006, 151:265-288.
[49]	Qiu Y M, Gao S, Mcnaughton N J, et al. First evidence of >3.2 Ga continental Crust in the Yangtze craton of South China and its implications for Archean Crustal evolution and phanerozoic tectonics[J]. Geology, 2000,28(1):11-14.
[50]	凌文黎,高山,张本仁,等.扬子陆核古元古代晚期构造热事件与扬子克拉通演化[J]. 科学通报, 2000, 45(21):2343-2348. [LING Wenli, GAO Shan, ZHANG Benren, et al. Yangtze continental Nuclear Late Paleoproterozoic tectonic thermal events and the evolution of the Yangtze craton[J]. Chinese Science Bulletin, 2000, 45(21):2343-2348.]
[51]	彭敏.扬子板块古元古代岩浆事件年龄及其地质意义[C]. 武汉:中国地质大学,2010:1-5.[PENG Min. PaleoProterozoic magmatism of Yangtze craton:timing and geological implications[C]. Wuhan:China University of Geosciences, 2010:1 -5.]
[52]	郭进京,张国伟,陆松年,等. 中国新元古代大陆拼合与Rodinia超大陆[J].高校地质学报,1999,5(2):148-154. [GUO Jinjing, ZHANG Guowei, LU Songnian, et al. Neoproterozoic continental block collage of China and Rodinia supercontinent[J]. Geological Journal of China Universities, 1999,5(2):148-154.]
[53]	陆松年,李怀坤,陈志宏,等. 新元古时期中国古大陆与罗迪尼亚超大陆的关系[J]. 地学前缘,2004,11(2):515-522. [LU Songnian, LI Huaikun, CHEN Zhihong, et al. Relationship between Neoproterozoic cratons of China and the Rodinia[J]. Earth Science Frontiers,2004,11(2):515-522.]
[54]	陆松年,李怀坤,陈志宏.塔里木与扬子新元古代热-构造事件特征、序列和时代-扬子与塔里木连接(TZ-TAR)假设[J]. 地学前缘,2003,10(4):321-326. [LU Songnian, LI Huaikun, CHEN Zhihong. Characteristics sequences and ages of Neoproterozoic thermo-tectonic events between Tarim and Yangtze blocks -a hypothesis of Yangtze-Tarim connection[J]. Earth Science Frontiers,2003,10(4):321-326.]
[55]	李献华,李武显,何斌. 华南陆块的形成与Rodinia超大陆聚合裂解观察解释与检验[J]. 矿物岩石地球化学通报,2012,31(6):543-559. [LI Xianhua, LI Wuxian, HE Bin. Building of the South China block and its relevance to assembly and breakup of Rodinia supercontinent:observations, interpretations and tests[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2012,31(6):543-559.]
[56]	Greentree M R,Li Z X. The oldest known rocks in southwestern China:SHRIMP U-Pb magmatic crystallization age and detrital provenance analysis of the Paleoproterozoic Dahongshan Group[J]. J. Asian Earth Sci.,2008,33:289-302.
[57]	Li Z H,Li X H,Zhou,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.
[58]	Duan L,Meng Q R,Zhang C L, et al.Tracing the position of the South China block in Gondwana U-Pb ages and Hf isotopes of Devonian detrital zircons[J]. Gondwana Research,2011,19;141-149.
[59]	Liu X,Gao S,Diwu C, et al. Precambrian crustal growth of Yangtze craton as revealed by detrital zircon studies[J]. AM.J.Science,2008,308:421-468.
[60]	Sun W H,Zhou M F,Gao J F, et al. Detrital zircon U-Pb geochronological and Lu-Hf isotopic constraints on the Precambrian magmatic and crustal evolution of the western Yangtze block, SW China[J]. Precam.Res., 2009, 172:99-126.
[61]	Sun W H, Zhou M F, Yan D P, et al. Provenance and tectonic setting of the Neoproterozoic Yanbian Group,western Yangtze block (SW China)[J]. Precam.Res.,2008,167:213-236.
[62]	Wang L J,Griffin W L, Yu J H, et al. Precambrian crustal evolution of the Yangtze block tracked by detrital zircons from Neoproterozoic sedimentary rocks[J]. Precam.Res.,2010,177:131-144.
[63]	Wang L J, Yu J H, Griffin W L,et al. Early crustal evolution in the western Yangtze block:evidence from U-Pb and Lu-Hf isotopes on detrital zircons from sedimentary rocks[J]. Precam.Res.,2012,222:368-385.
[64]	Wang X L, Zhou J C, Griffin W L, et al. Detrital zircon geochronology of Precambrian basement sequence in the Jiangnan orogen:Dating the assembly of the Yangtze and Cathaysia blocks[J]. Precam.Res.,2007,159:117-131.
[65]	Zhang S B, Zheng Y F,Wu Y B, et al. Zircon U-Pb age and Hf isotope evidence for 3.8Ga crustal remnant and episodic reworking of Archean crust in South China[J]. Earth Plant,2006,252:56-71.
[66]	Zhao Y F, Zhou M F, Li J W, et al. Late Paleoproterozoic to early Mesoproterozoic Dongchuan Group in Yunnan, SW China:Implication for tectonic evolution of the Yangtze block[J]. Precam.Res.,2010,182:57-69.
[67]	Zhao J H,Zhou M F, Yan D P, et al. Reappraisal of the ages of Neoproterozoic strata in South China:No connection with the Grenvillian orogeny[J]. Geology,2011,39;299-302.
[68]	程裕淇,王鸿祯.地球科学大词典[M]. 北京:地质出版社,2006:867.[CHENG Yuqi, WANG Hongzhen. Earth Science Dictionary[M]. Beijing:Geological Publishing House,2006:867.]
[69]	舒良树.华南前泥盆纪构造演化:从华夏地块到加里东期造山带[J]. 高校地质学报,2006,12(4):418-431. [SHU Liangshu. PreDevonian tectonic evolution of South China from Cathaysian block to Caledonian period folded orogenic belt[J]. Geological Journal of China Universities, 2006,12(4):418-431.]
[70]	舒良树.华南构造演化的基本特征[J]. 地质通报,2012,31(7):1035-1051. [SHU Liangshu. An analysis of principal features of tectonic evolution in South China block[J]. Geological Bulletin of China, 2012,31(7):1035-1051.]
[71]	Yao J L, Shu L S, Santosh M. Deteital zircon U-Pb geochronology, Hf-isotopes and geochemistry-New clues for the Precambrian crustal evolution of Cathaysia block, South China[J]. Gondwana Reseach,2011,20:553-567.
[72]	向磊,舒良树.华南东段前泥盆纪构造演化:来自碎屑锆石的证据[J]. 中国科学:地球科学, 2010, 40(10):1377-1388. [XIANG Lei, SHU Liangshu. Pre-Devonian tectonic evolution of the eastern South China Block:Geochronological evidence from detrital zircons[J]. Science China Earth China, 2010,40(10):1377-1388.]

[1]	XU Dailu, YIN Yong, SHI Lianqiang, LIN Wenrong, WANG Aihua, ZHENG Yujun. Sedimentary facies and environmental evolution of the Yangtze shoal, eastern China Sea shelf since Late Pleistocene: Evidence from core YZ05[J]. Marine Geology & Quaternary Geology, 2020, 40(6): 22-38. DOI: 10.16562/j.cnki.0256-1492.2019050501
[2]	CHEN Jianwen, XU Ming, LEI Baohua, SHI Jian, LIU Jun. Collision of North China and Yangtze Plates: Evidence from the South Yellow Sea[J]. Marine Geology & Quaternary Geology, 2020, 40(3): 1-12. DOI: 10.16562/j.cnki.0256-1492.2019070902
[3]	WANG Wenjuan, DOU Zhenya, CHEN Jianwen, ZHANG Yinguo, LIANG Jie. MARINE PALEO-MESOZOIC HYDROCARBON SOURCE ROCKS ON LAND OF THE LOWER YANGTZE PLATFORM AND THEIR IMPLICATIONS FOR OIL AND GAS EXPLORATION IN THE SOUTH YELLOW SEA BASIN[J]. Marine Geology & Quaternary Geology, 2017, 37(3): 138-146. DOI: 10.16562/j.cnki.0256-1492.2017.03.014
[4]	PANG Yumao, ZHANG Xunhua, XIAO Guolin, WEN Zhenhe, GUO Xingwei, SUN Jianwei, ZHAO Weina. COMPARATIVE STUDY OF TECTONIC EVOLUTION AND PETROLEUM GEOLOGICAL CONDITIONS OF TYPICAL SUPERIMPOSED BASINS IN UPPER AND LOWER YANGTZE BLOCK[J]. Marine Geology & Quaternary Geology, 2016, 36(1): 133-142. DOI: 10.3724/SP.J.1140.2016.01013
[5]	NIE Shiqi, HUANG Jinshui, LI Sanzhong. GLOBAL PLATE RECONSTRUCTION FROM ORDIVICIAN TO SILURIAN: KINEMATICS TEST OF THEIR LOCATIONS OF THREE CHINA'S CONTINENTS AND OCEAN-CONTINENT CONFIGURATION[J]. Marine Geology & Quaternary Geology, 2015, 35(4): 177-188. DOI: 10.16562/j.cnki.0256-1492.2015.04.019
[6]	YUE Baojing, LIAO Jing, LIU Hong, ZENG Jie, SHI Jian. EAST BOUNDARY OF THE COLLISION BELT BETWEEN SINO-KOREAN AND YANGTZE PLATES IN EASTERN CHINA AND THEIR EXTENSION IN THE SEA[J]. Marine Geology & Quaternary Geology, 2014, 34(1): 75-85. DOI: 10.3724/SP.J.1140.2014.01075
[7]	QI Jianghao, WEN Zhenhe, ZHANG Xunhua, FANG Nianqiao, GUO Xingwei. LITHOSTRATIGRAPHIC CORRELATION OF MESOZOIC AND PALAEOZOIC MARINE STRATA BETWEEN SOUTH YELLOW SEA AND UPPER YANGTZE REGION[J]. Marine Geology & Quaternary Geology, 2013, 33(1): 109-119. DOI: 10.3724/SP.J.1140.2013.01109
[8]	ZHANG Li, GENG Ansong, WANG Liaoliang, LIAO Yuhong, XU Guoqiang, WEI Zhenquan. ASSESSMENT OF MESOZOIC SOURCE ROCKS AT THE MARGIN OF SOUTH CHINA CONTINENT[J]. Marine Geology & Quaternary Geology, 2012, 32(1): 99-108. DOI: 10.3724/SP.J.1140.2012.01099
[9]	LIU Baoming, LIU Hailing. THE MESOZOIC IN THE SOUTH CHINA SEA AND ADJACENT AREAS: NEW TARGETS FOR HYDROCARBON EXPLORATION[J]. Marine Geology & Quaternary Geology, 2011, 31(2): 105-109. DOI: 10.3724/SP.J.1140.2011.02105
[10]	ZHANG Chong, WU Shi-min, QIU Xue-lin. FORMATION OF FORELAND BASINS IN THE SOUTH OF THE SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2007, 27(1): 61-70.

Cited By

Cited by

Periodical cited type(10)

1.	马赛婷，胡林，李明，王迪，陈林，程燕君，徐彬，吴智平. 珠江口盆地文昌A凹陷西部地区断裂体系的拓扑结构、分形特征及其与油气藏分布的关系. 高校地质学报. 2024(01): 36-46 .
2.	郑轩，宗兆云，付亚群，骆坤. 海域油气盖层叠前地震反演预测方法及应用. 吉林大学学报(地球科学版). 2024(06): 2128-2141 .
3.	黄俨然，唐宏宝，谭超，杨鹏宇，张炜，高钧健. 琼东南盆地松南低凸起潜山储层包裹体发育及油气成藏特征. 录井工程. 2024(04): 108-115 .
4.	罗泉源，焦祥燕，何小胡，王立锋，陈杨. 琼东南盆地西区黄流组重力流水道沉积特征及其控制因素. 海洋地质前沿. 2023(07): 25-33 .
5.	李鸿明，王璞珺，徐守立，刘迎松，吴仕玖，焦垚祺，王岩泉，刘亚南，宋国民，张艳. 琼东南盆地松南低凸起前古近系花岗岩潜山储层特征与控制因素. 世界地质. 2022(03): 568-582 .
6.	王真真，朱继田，李安琪，胡潜伟，毛雪莲，尹宏伟. 琼东南盆地新生代东西分块差异构造演化及控藏意义. 海洋地质与第四纪地质. 2021(04): 157-169 . 本站查看
7.	周欣，曹俊兴，王兴建，王俊，廖万平，杨金海. 琼东南盆地深水区松南区块新生代构造-沉积演化特征研究. 物探化探计算技术. 2021(05): 563-572 .
8.	罗泉源，焦祥燕，刘昆，李安琪，宋鹏. 乐东–陵水凹陷梅山组海底扇识别及沉积模式. 海洋地质与第四纪地质. 2020(02): 90-99 . 本站查看
9.	高永德，孙殿强，陈鸣，孙本强，刘博. 陵水17-2深水气田黄流组重力流沉积特征及模式. 中国海上油气. 2018(01): 22-30 .
10.	王彬，张强，吕福亮，杨涛涛，杨志力，孙国忠，吴敬武. 南海海域新生界沉积盆地天然气成藏条件及资源前景. 天然气地球科学. 2018(10): 1542-1552 .

Other cited types(2)

Get Citation

PDF

XML

Article views (1884) PDF downloads (17) Cited by(12)

Turn off MathJax

Article Contents

Abstract

References

TYPES AND CHARACTERISTICS OF THE CATHAYSIAN BLOCK GROUP