油气地质

滨里海盆地盐岩运动及相关圈闭类型

  • 毛明陆 ,
  • 杨亚娟 ,
  • 张艳
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  • 中国石化石油勘探开发研究院,北京 100083
史丹妮,1974 年生,女,硕士,现主要从事独联体地区油气地质方面的研究工作。E2mail:shdanni@sina.com.cn

网络出版日期: 2007-09-15

Salt movement and the types of related traps in Pre-Caspian Basin

  • MAO Minlu ,
  • YANG Yajuan ,
  • ZHANG Yan
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  • Research Institute of Petroleum Exploration and Development , Sinopec , Beijing 100083 , China

Online published: 2007-09-15

摘要

:位于东欧地台东南隅的滨里海盆地是世界上沉降最深、沉积厚度最大的含油气盆地之一,其中孔古尔阶盐岩地层及其与盐岩运动所产生的系列圈闭为该区盐上成藏及油气富集的重要因素。文中主要研究了该盆地盐岩分布、形态特征及盐岩运动演化历史,系统论述了与盐构造有关的油气圈闭类型及成因特征,为该盆地优选盐上勘探目标提供了科学依据。

本文引用格式

毛明陆 , 杨亚娟 , 张艳 . 滨里海盆地盐岩运动及相关圈闭类型[J]. 岩性油气藏, 2007 , 19(3) : 73 -79 . DOI: 10.3969/j.issn.1673-8926.2007.03.013

Abstract

Pre-Caspian Basin is one of the famous oil/ gas-bearing basin with the deepest subsidence and the thickest sedimentation in the world ,which is located in the southeastern East Europe Platform. The salt rock stratum in Kungurian of Lower Permian and the traps generated by salt movement are the main factors for post-salt reservoir accumulation and enrichment . The salt distribution , shape characteristics and the evolution of salt movement are studied ,and the types of hydrocarbon traps and genetic features are analyzed ,which provide scientific reference for the optimization of the exploration targets in post-salt strata.

参考文献

[ 1 ] 刘洛夫,朱毅秀,张占锋,等. 滨里海盆地盐上层的油气地质特征[J ]. 新疆石油地质,2002,23 (5):442-447.
[ 2 ] Alexander A C. Tectonic model for the evolution of the greater Caspian area [J ]. AAPG Bulletin,1999,83 (8).
[ 3 ] 童晓光. 世界石油勘探开发图集[M]. 北京:石油工业出版社,2004.
[ 4 ] 马克西莫夫C П. 苏联油气田手册[M]. 北京:石油工业出社,1992.
[ 5 ] Volozh Y, Talbot C, Ismail2Zadeh A T. Salt st2ructures and hydrocarbons in the Pricaspian basin [ J ]. AAPG Bulletin,2003,87 (3):313-334.
[ 6 ] 戈红星,Martin PA J ackson. 盐构造与油气圈闭及其综合利用[J ]. 南京大学学报(自然科学版),1996,32 (4):641-649.
[ 7 ] Khramov A N. Paleomagnetism and paleogeodynamics in the USSR(in Russian) [M]. Leningrad: VNIGRI,1991.
[ 8 ] Volozh Yu A,Sineli nikov A V,Groshev V G. Stratigraphy of Mesozoic-Cenozoic deposit s in the salt dome basin of the PreCaspian depression [ J ]. Stratigraphy and Geological Correlation,1996,4:409-415.
[ 9 ] Vendeville B C, J ackson M P A. The fall of diapirs during thin-skinned extensions [ J ]. Marine and Pet roleum Geology,1992,9 (8): 354-371.
[ 10 ] Alexander A C,Iwaniw E,Otto S C,et al. Tectonic model for the evolution of the Greater Caspian area (abs. ) [ C]. AAPG International Conference and Exhibition: Istanbul, Turkey,2000.
[ 11 ] Walsh J J,Watterson J,Nicol A,et al. Geomet ry and origin of a polygonal fault system[J ]. Journal of the Geological Society,2000,157:1261-1264.
[ 12 ] Watterson J,Walsh J J,Nicol A,et al. Geomet ry and origin of a polygonal fault system[J ]. Journal of the Geological Society,2000,157:151-162.
[ 13 ] Ismail Zadeh A T, Hupperth E,Lister J R. Gravitational and buckling instabilities of a rheologically layered st ruct ure: Implications for salt diapirism[J ]. Geophysical Journal International,2002,148 (2 ):288-302.
[ 14 ] J enyon M K. Salt tectonics[M]. London: Elsevier,1986. 174-179.
[ 15 ] 杰克逊M P A,盖洛韦W E 著. 墨西哥湾沿岸第三纪大陆边缘构造与沉积类型及其在油气勘探中的应用[M]. 刘民中译.北京:石油工业出版社,1988.

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