STUDY OF POSITIVE INVERSION STRUCTURES IN THE NORTH DEPRESSION OF THE SOUTH YELLOW SEA BASIN

LI Nan; LI Weiran; LONG Haiyan

doi:10.3724/SP.J.1140.2013.03095

2013 Vol. 33, No. 3

Article Contents

Abstract

References

Article navigation > Marine Geology & Quaternary Geology > 2013 > 33(3): 95-100

Next Article Previous Article

LI Nan, LI Weiran, LONG Haiyan. STUDY OF POSITIVE INVERSION STRUCTURES IN THE NORTH DEPRESSION OF THE SOUTH YELLOW SEA BASIN[J]. Marine Geology & Quaternary Geology, 2013, 33(3): 95-100. doi: 10.3724/SP.J.1140.2013.03095

Citation:

LI Nan, LI Weiran, LONG Haiyan. STUDY OF POSITIVE INVERSION STRUCTURES IN THE NORTH DEPRESSION OF THE SOUTH YELLOW SEA BASIN[J]. Marine Geology & Quaternary Geology, 2013, 33(3): 95-100. doi: 10.3724/SP.J.1140.2013.03095

STUDY OF POSITIVE INVERSION STRUCTURES IN THE NORTH DEPRESSION OF THE SOUTH YELLOW SEA BASIN

College of Marine Geosciences, Ocean University of China, Qingdao 266100, China

Received Date: 07 February 2012

Revised Date: 20 September 2012

Abstract

Abstract

Several types of positive inversion structures are developed in the Cenozoic strata of the Northeast Sag, North Sag, Middle Sag and South Sag in the North Depression of the South Yellow Sea Basin, including penetrated fault-propagation type, compressive fold type, reversed fault type, and so on. Oligocene and the end of Pliocene are the two main inversion periods, and the structural inversion in Oligocene is more obvious. The convergence rate between the Pacific Plate and Eurasia Plate is an important factor controlling the development of inversion structures in Cenozoic in the North Depression of the South Yellow Sea Basin. The positive inversion structures are favorable to hydrocarbon accumulation and unfavorable to hydrocarbon preservation if the intensity of tectonic inversion is great.
- inversion structure /
- structural style /
- South Yellow Sea Basin /
- convergence rate

FullText(HTML)

References

[1]	Glennie K W,Boeger P L. Sole pit Inversion Tectonics[C]//Petroleum Geology of the Continental Shelf of Northwest Europe.1984:110-120. Google Scholar
[2]	Cooper M A, Williams G D. Inversion Tectonics[M]. London:Geological Society Special Publication,1989:5-11. Google Scholar
[3]	Mitra S. Geometry and kinematic evolution of inversion structures[J].AAPG Bulletin,1993,77(7):1159-1191. Google Scholar
[4]	胡望水,吕炳全,毛治国,等.中国东部中新生代含油气盆地的反转构造[J].同济大学学报,2004,32(2):182-186. Google Scholar [HU Wangshui, LU Bingquan,et al. Inversion structure characteristic of petroleum basin in Mesozoic and Cenozoic in Middle and East China[J]. Journal of Tongji University,2004,32(2):182-186.] Google Scholar
[5]
[6]	侯方辉,张志珣,张训华,等.南黄海盆地地质演化及构造样式地震解释[J].海洋地质与第四纪地质,2008,28(5):61-68. Google Scholar [HOU Fanghui, ZHANG Zhixun, ZHANG Xunhua, et al. Geologic evolution and tectonic styles in the South Yellow Sea basin[J]. Marine Geology and Quaternary Geology,2008,28(5):61-68.] Google Scholar
[7]	Hayward A B, Graham H R. Some Geometrical Characteristics of Inversion[M]. Geological Society Special Publication,1989:34-56. Google Scholar
[8]	刘和甫.伸展构造及其反转作用[J].地学前缘,1995,2(1):113-123. Google Scholar [LIU Hefu. Extensional tectonics and its inversion[J].Earth Science Frontiers,1995,2(1):113-123.] Google Scholar
[9]	陈昭年,陈发景.反转构造与油气圈闭[J].地学前缘,1995,2(3-4):96 Google Scholar -102.[CHEN Zhaonian, CHEN Fajing. Inversion structures and their relationship to traps of oil and gas[J]. Earth Science Frontiers,1995,2(3-4):96-102.] Google Scholar
[10]	蔡乾忠.中国海域油气地质学[M].北京:海洋出版社,2005:131-150.[CAI Qianzhong. Oil and Gas Geology in China Seas[M].Beijing:China Ocean Press,2005:131 Google Scholar -150.] Google Scholar
[11]	姚永坚,夏斌,冯志强.南黄海古生代以来构造演化[J].石油实验地质,2005,27(2):124-128. Google Scholar [YAO Yongjian, XIA Bin, FENG Zhiqiang. Tectonic evolution of the South Yellow Sea since the Paleozoic[J]. Petroleum Geology and Experiment, 2005,27(2):124-128.] Google Scholar
[12]	吴珍汉.中国大陆及邻区新生代构造-地貌演化过程与机理[M].北京:地质出版社,2001:203-207.[WU Zhenhan. Cenozoic Tectonics in China Mainland and Its Adjacent Regions-Process and Mechanism of the Geomorphic Evolution[M].Beijing:Geological Publishing House,2001:203 Google Scholar -207.] Google Scholar
[13]	汪新文.中国东北地区中-新生代盆地构造演化与油气关系[M].北京:地质出版社,2007:105-115.[WANG Xinwen. Relationship between Structural Evolution and Petroleum of Mesozoic-Cenozoic Basins in Northeast China[M]. Beijing:Geological Publishing House, 2007:105 Google Scholar -115.] Google Scholar
[14]	任建业,李思田.西太平洋边缘海盆地的扩张过程和动力学背景[J].地学前缘,2000,7(3):203-211. Google Scholar [REN Jianye, LI Sitian. Spreading and dynamic setting of marginal basins of the Western Pacific[J]. Earth Science Frontiers, 2000,7(3):203-211.] Google Scholar
[15]	Jurdy D M. Relative plate motions and the formation of marginal basins[J]. Geophys. Res., 1979, 84(B12):6796-6802. Google Scholar
[16]	Cox A, Engebretson D.Change in motion of Pacific Plate at 5 Myr BP[J]. Nature, 1985,313(6002):472-474. Google Scholar
[17]	Northrup C J, Royden L H, Burchfiel B C. Motion of the Pacific Plate Relative to Eurasia and Its Potential Relation to Cenozoic Extension along the Eastern Margin of Eurasia[J]. Geology,1995, 23(8):719-722. Google Scholar
[18]	宁飞,汤良杰,张钰,等.塔中隆起早古生代反转构造及其石油地质意义[J].石油与天然气地质,2010,31(1):57-62. Google Scholar [NING Fei, TANG Liangjie, ZHANG Yu, et al. Eopaleozoic inversion structures in the Tazhong Uplift and their significance to petroleum geology[J].Oil & Gas Geology, 2010,31(1):57-62.] Google Scholar

Relative Articles

[1]	LI Nan, LI Weiran, LONG Haiyan. STUDY OF POSITIVE INVERSION STRUCTURES IN THE NORTH DEPRESSION OF THE SOUTH YELLOW SEA BASIN. Marine Geology & Quaternary Geology, 2013, 33(3): 95-95. doi: 10.3724/SP.J.1140.2013.03095
[2]	XIONG Zhong, JIANG Zhiqiang, SUN Peng, TAN Sizhe, XU Zhenzhong, CHEN Wenxia. Characteristics and tectonic evolution of the fault system in the north sag of Northern Depression of South Yellow Sea basin. Marine Geology and Quaternary Geology, 2018, 38(3): 75-75. doi: 10.16562/j.cnki.0256-1492.2018.03.007
[3]	WANG Lifei, GUO Lihua, NIE Xin. STRUCTURAL FEATURES AND EVOLUTIONARY STAGES OF THE WESTERN DEPRESSION OF THE NORTH YELLOW SEA BASIN. Marine Geology & Quaternary Geology, 2012, 32(3): 55-55. doi: 10.3724/SP.J.1140.2012.03055
[4]	GONG Chenglin, LEI Huaiyan, WANG Yingmin, LIU Zhenhu, GUAN Baocong, HU Xiaoqiang, LU Jinbo. HYDROCARBON GEOLOGIC CHARACTERS AND STRUCTURAL EVOLUTION IN THE EASTERN DEPRESSION OF NORTH YELLOW SEA BASIN. Marine Geology & Quaternary Geology, 2009, 29(1): 79-79. doi: 10.3724/SP.J.1140.2009.01079
[5]	LI Xutong, WU Zhiqiang, ZHANG Xunhua. PETROLEUM GEOLOGY OF THE CRETACEOUS IN THE NORTHERN DEPRESSION OF SOUTH YELLOW SEA BASIN: EVIDENCE FROM SEISMIC ATTRIBUTE ANALYSIS. Marine Geology & Quaternary Geology, 2015, 35(6): 119-119. doi: 10.16562/j.cnki.0256-1492.2015.06.012
[6]	WANG Lifei, WANG Yantang, HU Xiaoqiang. STRATIGRAPHY AND SEDIMENTARY CHARACTERS OF THE WESTERN DEPRESSION,NORTH YELLOW SEA BASIN. Marine Geology & Quaternary Geology, 2010, 30(3): 97-97. doi: 10.3724/SP.J.1140.2010.03097
[7]	LIANG Jie, WEN Zhenhe, XIAO Guolin, ZHANG Yinguo, ZHAO Qingfang, DONG Heping, LI Qing. THE IMPACT OF HYDROTHERMAL ACTIVITY ON THE RESERVOIRS IN THE EAST DEPRESSION OF THE NORTH YELLOW SEA BASIN. Marine Geology & Quaternary Geology, 2015, 35(5): 117-117. doi: 10.16562/j.cnki.0256-1492.2015.05.014
[8]	LIANG Jie, WEN Zhenhe, XIAO Guolin, ZHANG Yinguo, DONG Heping. RESERVOIR CHARACTERISTICS AND INFLUENTIAL FACTORS IN THE EASTERN DEPRESSION OF THE NORTH YELLOW SEA BASIN. Marine Geology & Quaternary Geology, 2013, 33(2): 111-111. doi: 10.3724/SP.J.1140.2013.02111