从东海石油地质工作的重要进展看西太平洋大陆边缘新生代盆地的构造演化——一种海沟向洋后退的残余弧后盆地的演化模式

孙肇才

doi:10.11781/sysydz200402121

从东海石油地质工作的重要进展看西太平洋大陆边缘新生代盆地的构造演化——一种海沟向洋后退的残余弧后盆地的演化模式

doi: 10.11781/sysydz200402121

孙肇才

中国石化石油勘探开发研究院, 无锡实验地质研究所, 江苏, 无锡, 214151

详细信息

作者简介:
孙肇才(1932- ),男(汉族),山东济南人,教授级高级工程师,主要从事石油地质研究工作.

中图分类号: TE121.2
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出版历程
- 收稿日期: 2003-09-26
- 刊出日期: 2004-03-25

RETHINKING ABOUT THE TECTONIC EVOLUTION OF THE CENOZOIC CONTINENTAL MARGINAL BASIN OF THE WEST PACIFIC OCEAN IN ACCORDANCE WITH SOME IMPORTANT ADVANCES OF STUDIES OF PETROLEUM GEOLOGY IN EAST CHINA SEA——AN EVOLUTIONARY MODEL OF RESIDUAL BACK ARC BASINS DEVELOPED IN THE LOCATION OF TRENCHES RETREATING TOWARDS THE OCEAN

SUN Zhao-cai

Wuxi Research Institute of Experimental Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214151, China

摘要

摘要: 中国所在的亚洲,是全球地质结构最复杂的一个洲.这里不仅有若干小地块与巍峨造山带形成的镶嵌组合,还有以沟、弧、盆并行发育的长达近20000km的现代大陆边缘.中国地质学家,以黄汲清、朱夏院士作代表,先后以"多旋回"、"3个构造域"(古亚洲、滨太平洋及特提斯—喜马拉雅)和"东西两条锋线"等简明的概括,对中国地质构造以大陆内部为主的内涵,进行了深邃的阐述.在他们的影响之下,力图以简介东海石油地质进展为契机,在"海沟向洋后退和残余弧后盆地"思想下,对西太平洋大陆边缘的构造演化及盆地发生规律,作一个尝试性的探讨,并以此来纪念黄汲清院士诞辰100周年.
- 大陆边缘 /
- A型及B型俯冲 /
- 岛弧向洋后退 /
- 残余弧后盆地
Abstract: Asia is the most complicated continent in the view of global geological tectonics.There is not only mosaic structures consisting of small blocks and giant orogenic belts,but also modern continental margin with trenchs,island arc and basins lasting for 20 000 km.Chinese geologists,presented by Academian Huang Jiqing and Zhu xia,elaborated the geological tectonics of China by theories of "polycycle","three tectonic domains (PaleoAsian,marginal-Pacific and Tethyan-Himalayan tectonic domains)"and "two frontal lines both in west and east".Under the light of their theories,the tectonic evolution of continental margin of west Pacific ocean and the development of basins in the area were studied with the idea of "trench retreating towards ocean and residual backarc basins",which was in accordance with some important advances of studies of petroleum geology in East China Sea.
- continental margin /
- A-type and B-type subduction /
- island arc retreating towards ocean /
- residual backarc basin

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参考文献(20)

[1]	Dickinson W R.Plate tectonic evolution of sedimentary basins [A].Plate tectonics and hydrocarbon accumulation [C].AAPG short course,1979.1-56.
[2]	许靖华(何起祥译).地学革命风云录[M].北京:地质出版社,1985.77-99.
[3]	Kenneth J Hsu.Origin of sedimentary basin of China[A].Sedimentary Basins of the World[C].1989.207-227.
[4]	陈桂华,李友川,付宁,等.平湖油气田油气分布主控因素分析[J].中国海上油气(地质),2003,17(3):164-169.
[5]	Karig D E.Origin and development of marginal basins in western Pacific[J].Journal of Geophysical Reasearch,1971,76(2):2 542-2 561.
[6]	Gerhrd Einsele.Remnant and Foreland Basins[A].Sedimentary Basins (Second)[C].1991.606-621.
[7]	Tapponier P.Propagating extrusion in Asia:new insights from simple experiments with plassticize[J].Geology,1982,10(2):611-616.
[8]	FuKao Y,Maruyama S,et al.Geologic implication of the whole mantle P-wave tomorgraphy [J].Geol Soc Japan,1994,100(2):4-23.
[9]	孙肇才.政策、思路和选区——就发展我国天然气在中国科学院地学部会议上发言摘要[J].石油实验地质,1989,11(3):301-312.
[10]	孙肇才.中国含油气盆地基本地质特征[J].海洋地质与第四纪地质,1991,11(3):1-14.
[11]	朱夏.中国东部板块内部盆地形成机制的初步探讨[A].朱夏论中国含油气盆地构造[C].北京:石油工业出版社,1986.35-43.
[12]	姚伯初,曾维军,Hayes D E等.中美合作调研南海地质专报[M].武汉:中国地质大学出版社,1994.1-191.
[13]	姚伯初.大陆岩石圈在张裂和分离时的变形模式[J].海洋地质与第四纪地质,2002,22(3):59-66.
[14]	徐克定,吴根耀,马力,等.中国南方构造研究新进展及其基本格架[A].油气盆地研究新进展[C].北京:石油工业出版社,2002.180-194.
[15]	M, G 奥德利-查尔斯,M 拉特雷那,GAS 纳恩.喜马拉雅到东亚岛弧特提斯造山带[A].特提斯构造带地质学——廿六届国际地质大会论文选译[C].北京:地质出版社,1983.48-57.
[16]	Lallemand S.东南亚正在活动的俯冲与碰撞作用[J].石油地质与实验,2002,(2):1-5.
[17]	Viallon C.冲绳海槽的开启和台湾的碰撞:一种具有侧向固定翼的海沟后退模式[J].石油地质与实验,2002,(2):39-47.
[18]	孙肇才.前陆类盆地的风格与共性——以中国中西部中新生代陆内前陆盆地为例[A].板内形变与晚期成藏——孙肇才石油地质论文选[C].北京:地质出版社,2003.104-128.
[19]	邓属予.台湾第三纪陆缘盆地的构造演化[J].石油实验地质,2002,(2):22-32.
[20]	Forschungsschiff sonne.Geol Jb,Reihe D,Heft 93.1991.226-229.