伏尔加—乌拉尔典型前陆盆地石油地质特征及勘探前景分析

李斌; 朱筱敏

doi:10.11781/sysydz201201047

伏尔加—乌拉尔典型前陆盆地石油地质特征及勘探前景分析

doi: 10.11781/sysydz201201047

李斌^1,2,
朱筱敏^1,2

1.
中国石油大学(北京)油气与资源探测国家重点实验室, 北京, 102249
2. 中国石油大学(北京)地球科学学院, 北京, 102249

基金项目: 中石油基金项目“全球剩余油气资源研究及油气资源快速评价技术”(2008ZX05028-003)资助

详细信息

作者简介:
李斌(1970- ),男,博士后.从事沉积学及空间数据库研究.E-mail:libin9600@sohu.com.

中图分类号: P618.13
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出版历程
- 收稿日期: 2011-03-28
- 修回日期: 2011-12-13
- 刊出日期: 2012-01-28

Petroleum geology and exploration potential of Volga-Ural Basin：one typical foreland

Li Bin^1,2,
Zhu Xiaomin^1,2

1.
State Key Laboratory of Petroleum Resource Prospecting, China University of Petroleum, Beijing 102249, China
2. Earth Sciences Institute, China University of Petroleum, Beijing 102249, China

摘要

摘要: 伏尔加—乌拉尔盆地为东欧地台东部边缘一个典型的前陆盆地,发育前寒武里菲纪—新生代第四纪地层,其中上古生界海相碳酸盐岩地层中发育良好的生、储、盖组合,形成了巨型富油气区,具有广阔的油气资源前景。其构造演化经历了陆内裂谷碎屑岩阶段、被动陆缘碳酸盐岩台地阶段、造山带前陆盆地形成阶段以及前陆盆地碎屑岩阶段。研究表明,该盆地经历了大陆开裂—大陆碰撞整个"威尔逊旋回"的构造运动,具有典型的大型前陆盆地形成与演化特征;被动陆缘阶段发育的生物碳酸盐岩为烃源岩提供了物质基础,而在前陆盆地形成时造山带强烈的区域构造运动为油气运移提供了动力,使油气大规模聚集;盆地东部褶皱带为今后重要的勘探区。
- 石油地质 /
- 碳酸盐台地 /
- 被动陆缘 /
- 前陆盆地 /
- 伏尔加—乌拉尔盆地
Abstract: The Volga-Ural Basin is a typical foreland basin in the eastern margin of the Eastern Europe Platform.Subsidence continued from Riphean of pre-Cambrian to Quaternary of Cenozoic.Good assemblages of source rock,reservoir and seal exist in the marine facies carbonate rocks of the middle and upper Paleozoic,resulting in giant petroliferous region which has great potential for petroleum exploration.The tectonic evolution of the basin can be divided into four stages including:1) clastic rock in intracontinental rift;2) carbonate tableland in passive margin;3) foreland basin of orogenic belt;4) clastic rock in foreland basin.Studies show that the basin has underwent a complete"Wilson Circle"from continent rift to continent collision,and is regarded as a typical giant foreland basin.Biological carbonate rocks generated during the passive margin stage contributed to hydrocarbon generation.Severe regional tectonic movements of orogenic belt when foreland basin formed provided driving force for petroleum migration and accumulation.Folds in the east of the basin are targets for future exploration.
- petroleum geology /
- carbonate tableland /
- passive margin /
- foreland basin /
- Volga-Ural Basin

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参考文献(27)

[1]	陈昭国,曾凝.前陆盆地概述及其与油气关系:兼论四川前陆盆地的形成[J].四川地质学报,1996(3):219-223.
[2]	何辉,樊太亮,林琳,等.巴西亚马逊盆地石油地质特征及勘探前景分析[J].西南石油大学学报(自然科学版),2010,32(3):61-66.
[3]	高小惠,唐波,李锦华.哥伦比亚上马格达莱纳盆地油气地质特征[J].断块油气田,2010,17(3):262-265.
[4]	吴因业,邹才能,胡素云,等.全球前陆盆地层序沉积学新进展[J].石油与天然气地质,2011,32(4):606-614.
[5]	Dickinson W R.Sedimentary basin developed during evolution of the Mesozoic:Cenozoic[J].Can J Earth Sci,1976,13:1268-1288.
[6]	Moss S T,Mccarthy A J.Foreland basin systems(discussion)[J].Basin Research,1997,9:171-176.
[7]	Flemmings P B,Jordan T E.Stratigraphic modelling of foreland basin:interpreting thrust defo rmation and litho sphererheology[J].Geology,1990,18:430-434.
[8]	Flemmings P B,Jordan T E.A synthetic stratigraphic model of foreland basin development[J].Journal of Geophysical Research,1989,94(B4):3851-3866.
[9]	Houseknecht D W.Evolution from passive margin to foreland basin:the atoka formation of the Arkoma Basin,South central U.S.A.[M]//Allen P A,Homewood P.eds.Foreland Basin.New York:John Wiley & Sons,Inc.,1986:327-345.
[10]	Watts A B,Kaner G,Steck ler M.Litho sphere flexure and the evolution of sedimentary basin[J].Philosophical Transactions of the Royal Society of Lond on(Series A),1982,305:249-281.
[11]	Dickinson W R.板块构造与油气聚集[M].郝石生,刘和甫,译.北京:石油工业出版社,1981:1-42.
[12]	Klein G D.Current aspects of basin analysis[J].Sedimentary Geology,1987,50:90-118.
[13]	Dickinson WR.Plate tectonics and hydrocarbon accummulation[C]//AAPG continuing education course note series.New Orleans:AAPG,1976:1-56.
[14]	Bally A W.Basin and subsidence:a summary[C]//Bally A W,ed.Dynamics of plate interiors.American Geophysical Union and Geological Society of Geo-dynamics Series 1,1980:5-20.
[15]	Klein GD.Current aspects of basin analysis[J].Sedimentary Geology,1987,50:90-118.
[16]	牟琨,云金表.准噶尔盆地腹部隐蔽油气藏类型与成藏主控因素[J].石油实验地质,2010,32(2):154-158.
[17]	潘春孚,纪友亮,高志勇,等.准噶尔盆地南缘新近系层序类型与发育模式研究[J].断块油气田,2011,18(1):34-37.
[18]	张渝昌.中国含油气盆地原型分析[M].南京:南京大学出版社,1997:50-60.
[19]	徐旭辉,高长林,黄泽光,等.中国盆地形成的三大活动构造历史阶段[J].石油与天然气地质,2005,26(2):155-162.
[20]	Brown D,Spadea P,Puchkov V,et al.Arc--continent collision in the Southern Urals[J].Earth-Science Reviews,2006,79:61-287.
[21]	IHS.IHS Basin Mortor urals foredeep province Basin(VolgaUrals)[R].[S.l.] :IHS,2008:1217.
[22]	Aliyev M M,Morozov S G,Postnikova I Y,et al.Geology and oil and gas occurrence in Riphean and Vendian deposits in the Volga Urals province.1977:156.
[23]	Bogdanov M M,Rile Y B.Some paleotectonic characteristics of the formation of hydrocarbon pools in Devonian sub reef structures of the north of the Volga Ural Province[J].Petroleum Geology,1984:20(9):427-429.
[24]	Nartov G V.Tectonic and facies criteria for the distribution of Upper Devonian Toumaisian organic buildups in the south of the Ural Volga region[J].Petroleum Geology,1986,21(10):465-468.
[25]	Mart Y,Ryan W B F,Lunina O V.Review of the tectonics of the Levant Rift system:the stru ctural significance of oblique continental breakup[J].Tectonophysics,2005,395:209-232.
[26]	Morgan W J.Hot tracks and the opening of the Atlantic and Indian Oceans[M]//Emiliani C.The sea.New York:Wiley Interscience,1981:443-487.
[27]	Lister G S,Etheridge M A,Symonds P A.Detachment faulting and the evolution of passive cont inental margins[J].Geology,1986,14:246-250.