中国西部复杂叠合盆地油气成藏研究进展与问题

doi:10.11867/j.issn.1001-8166.2007.09.0879

地球科学进展 ›› 2007, Vol. 22 ›› Issue (9): 879 -887. doi: 10.11867/j.issn.1001-8166.2007.09.0879

973项目研究进展下一篇

中国西部复杂叠合盆地油气成藏研究进展与问题

庞雄奇 ¹,罗晓容 ²,姜振学 ¹,林畅松 ³,张水昌 ⁴,钟宁宁 ¹,李忠 ²

1．中国石油大学，北京 102249; 2．中国科学院地质与地球物理研究所，北京 100029;3．中国地质大学，北京 100083; 4．中国石油勘探开发研究院，北京 100083

收稿日期:2007-07-20 修回日期:2007-08-21 出版日期:2007-09-15
通讯作者: 庞雄奇(1961-),男,湖北崇阳人，教授,博士生导师，主要从事油气藏形成与分布、盆地定量分析与油气资源评价的教学和研究工作.E-mail:pangxq@cup.edu.cn E-mail:pangxq@cup.edu.cn
基金资助:
国家重点基础研究发展计划项目“中国典型叠合盆地油气形成富集与分布预测”（编号：G1999043300）资助.

Advancements and Problems on Hydrocarbon Accumulation Research of Complicated Superimposed Basins in Western China

PANG Xiong-qi ¹, LUO Xiao-rong ², JIANG Zhen-xue ¹, LIN Chang-song ³, ZHANG Shui-chang ⁴, ZHONG Ning-ning ¹, LI Zhong ²

1. China University of Petroleum, Beijing 102249,China；2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029,China；3. China University of Geosciences,Beijing 100083,China；4. CNPC Research Institute of Petroleum Exploration and Production, Beijing 100083,China

Received:2007-07-20 Revised:2007-08-21 Online:2007-09-15 Published:2007-09-10

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中国西部复杂叠合盆地富集了中国45%左右的剩余油气资源，目前探明率不到20%，发展潜力巨大。近20年来的基础理论研究表明，中国西部复杂叠合盆地具有“多期构造变革、多套生储盖组合、多旋回油气成藏、多次调整改造”的油气地质特征，大油气田的形成和分布受“古隆起迁移、烃源灶演化、区域盖层发育、构造平衡带叠合”四大要素的控制，在此基础上提出了“多元复合—过程叠加”的成藏模式和有利勘探区预测方法，为塔里木盆地的油气勘探进一步指明了方向。除四大要素外，复杂油气藏的形成和分布还受“圈闭发育分布”、“储层发育分布”、“优势通道形成演化”、“运聚动力条件”及其相互耦合关系的控制，在已有成果的基础上进一步开展“复杂油气藏形成演化机制与分布规律”的基础研究，对于进一步提高钻探成效和发展叠合盆地油气勘探理论具有重大的现实意义。

关键词: 油气藏形成, 复杂叠合盆地, 油气田勘探, 油气预测

About 45% of China's remaining hydrocarbon resources are contained in the complicated superimposed basins in western China. However, the proven ratio is less than 20% and the potential is great. The researches of basic theories over the past two decades indicate that these superimposed basins are characterized by four geological features: “multi-phase structural revolution, multi-sets of source-reservoir-seal assemblages, multi-cycles of hydrocarbon accumulation and multi-phase adjustment and reconstruction”. The formation and distribution of giant fields are controlled by four key elements including “the migration of paleo-highs, the evolution of source kitchens, the development of regional seals and the superimposition of structural equilibrium belts. Based on the research results, the accumulation model of ”multi factors recombination and process superimposition" and the methodology for predicting favorable exploration fairways are proposed to guide the hydrocarbon exploration in the Tarim basin. Besides the four key elements mentioned above, the formation and distribution of complicated hydrocarbon accumulations are also controlled by “development and distribution of traps, development and distribution of reservoir rocks, formation and evolution of preferential migration pathways, dynamic conditions for migration and accumulation” and their inter-coupling relationships. Based on the previous achievements, further basic researches on “formation and evolution mechanism and distribution patterns of complicated hydrocarbon accumulations” has a great practical significance to improve the efficiency of exploration drilling and develop exploration theories on petroleum explorations in superimposed basins.

Key words: Complicated superimposed basin, Hydrocarbon prediction., Formation of hydrocarbon accumulations, Petroleum exploration

中图分类号:

TE121.1

[1]Bally A W，Snelson S.Realms of subsidence[J]．Canadiam Society of Petroleum Geologists Memory，1980，6：9-94.
[2]Liu Guangding. Preliminary discussion on Residual basins [J].China Petroleum Exploration,1997,2（3）:1-4.[刘光鼎．试论残留盆地[J]．勘探家，1997，2（3）：1-4.]
[3]Liu Chiyang,Yang Xingke. Thinking for researches and oil-gas assessment of reformed basins [J].Oil and Gas Geology,2000,21（1）:11-14.[刘池洋，杨兴科．改造盆地研究和油气评价思路[J]．石油与天然气地质，2000，21（1）：11-14.]
[4]Liu Chiyang,Sun Haishan. Classification of reformed basin[J].Xinjiang Petroleum Geology,1999,20（2）:79-83.[刘池洋，孙海山．改造型盆地类型划分[J]．新疆石油地质，1999，20（2）：79-83.]
[5]Zhao Wenzhi, He Dengfa. Concept and its significance of composite petroleum systems in China[J].China Petroleum Exploration,2000,5（3）:1-11.[赵文智，何登发．中国复合含油气系统的概念及其意义[J].勘探家，2000，5（3）：1-11.]
[6]Wang Qingchen, Jin Zhijun. Superimposed basin and oil-gas’ ormation and accumulation[J].China Basic Science,2002,6:4-7.[王清晨，金之钧．叠合盆地与油气形成富集[J]．中国基础科学，2002，6：4-7.]
[7]He Dengfa, Jia Chengzao. Discussion and analysis of superimposed sedimentary basins[J].Petroleum Exploration and Development,2004,31(1) :1-5.[何登发，贾承造．叠合盆地概念辨析[J]．石油勘探与开发，2004，31(1)：1-5.]
[8]Tang Liangjie, Jin Zhijun, Pang Xiongqi. Hydrocarbon migration and accumulation models of superimposed basins[J].Journal of the University of Petroleum, China (Edition of Natural Science),2000,24（4）:67-71.[汤良杰，金之钧，庞雄奇．多期叠合盆地油气运聚模式[J]．石油大学学报:自然科学版，2000，24（4）：67-71.]
[9]Jia Chengzao. Structural characteristics and oil/gas accumulative regularity in Tarim basin[J].Xinjiang Petroleum Geolgoy,1999,20（3）:177-183.[贾承造．塔里木盆地构造特征与油气聚集规律[J]．新疆石油地质，1999，20（3）：177-183.]
[10]Jia Chengzao. Tectonic Characteristics and Hydrocarbon in the Tarim Basin of China[M]. Beijing: Petroleum Industry Press,1997:1-424.[贾承造．中国塔里木盆地构造特征与油气[M]．北京：石油工业出版社，1997:1-424.]
[11]Tang Liangjie, Jin Zhijun, Jia Chengzao,et al. Tectonic analysis of superimposed basins[J].Experimental Petroleum Geology,2001,23(3):251-255.[汤良杰,金之钧,贾承造,等.叠合盆地构造解析几点思考[J].石油实验地质，2001,23(3)：251-255.]
[12]Tian Zaiyi. The Controlling Factors for Hydrocarbon Enrichment in Sedimentary Basin[C]//Tian Zaiyi Petroleum Geological Papers Collection.Beijing: Petroleum Industry Press,1997.[田在艺．沉积盆地控制油气赋存的因素[C]//田在艺石油地质论文选集.北京：石油工业出版社，1997.]
[13]Pang Xiongqi, Jin Zhijun, Jiang Zhenxue,et al. Evaluation of hydrocarbon resources of superimposed basin and its significance [J].Petroleum Exploration and Development,2002,29（1）:9-13.[庞雄奇，金之钧，姜振学,等．叠合盆地油气资源评价问题及其研究意义[J]．石油勘探与开发，2002，29（1）：9-13.]
[14]Kang Yuzhu. Geological condition for forming big gas fields in Tarim basin[J].Oil and Gas Geology,2001,22（1）:21-25.[康玉柱．塔里木盆地大气田形成的地质条件[J]．石油与天然气地质，2001，22（1）：21-25.]
[15]Chen Jianfa, Zhang Shuichang, Sun Shengli.Main factors influencing marine carbonate source rock formation[J].Acta Geologica Sinica,2006,80（3）:467-472.[陈践发,张水昌,孙省利,等.海相碳酸盐岩优质烃源岩发育的主要影响因素[J].地质学报，2006,80（3）：467-472.]
[16]Jin Zhijun, Yang Lei, Zeng Jianhui,et al.Deep fluid activities and their effects on generation of hydrocarbon in Dongying depression[J].Petroleum Exploration and Development,2002,29（4）:42-44.[金之钧，杨雷，曾溅辉.东营凹陷深部流体活动及其生烃效应初探[J].石油勘探与开发，2002,29（4）：42-44.]
[17]Jin Zhijun, Zhang Liuping, Zeng Jianhui,et al.The composite-origin hydrocarbon related with mantle-derived CO₂ enriching fluid in Dongying depression[J].Chinese Science Bulletin,2002,47（16）:1 276-1 280.[金之钧,张刘平，曾溅辉,等.东营凹陷与慢源富CO₂流体有关的复合成因烷烃[J].科学通报，2002,47（16）：1 276-1 280.]
[18]Pang Xiongqi, Jin Zhijun, Zuo Shengjie. Dynamics models and classification of hydrocarbon accumulations[J].Earth Science Frontiers,2000,7（4）:507-513.[庞雄奇，金之钧，左胜杰．油气藏动力学成因模式与分类[J]．地学前缘，2000，7（4）：507-513.]
[19]Pang Xiongqi. Hydrocarbon Expulsion Threshold Controlling Hydrocarbon Theory and Its Applicatoin[M].Beijing:Petroleum Industry Press,1995.[庞雄奇．排烃门限控油气理论及应用[M]．北京：石油工业出版社，1995.]
[20]Lü Xiuxiang, Zhang Yiwei, Jin Zhijun. Study on accumulation cycle in Tarim basin[J].Chinese Science Bulletin,1996,41（22）:2 064-2 066.[吕修祥，张一伟，金之钧．塔里木盆地成藏旋回初论[J]．科学通报，1996，41（22）：2 064-2 066.]
[21]Zhou Haiyan ,Pang Xiongqi, Jiang Zhenxue. Hydrocarbon accumulation threshold and its study methods[J].Acta Petrolei Sinica,2003,24(6):40-44.[周海燕，庞雄奇，姜振学.油气成藏门限及其研究方法[J].石油学报,2003,24(6)：40-44.]
[22]Jin Zhijun. New progresses in research of China’s typical superimposed basins and reservoiring of hydrocarbons (Part Ⅰ): Taking Tarim basin as an example[J]. Oil and Gas Geology,2005,26(5):553-560.[金之钧.中国典型叠合盆地及其油气成藏研究新进展(1)[J].石油与天然气地质，2005,26(5)：553-560.]
[23]Jin Zhijun. New progresses in research of China's typical superimposed basins and reservoiring of hydrocarbons (Part Ⅱ): Taking Tarim basin as an example[J].Oil and Gas Geology,2006,27(3):281-288.[金之钧.中国典型叠合盆地及其油气成藏研究新进展(2)[J].石油与天然气地质，2006,27(3)：281-288.]
[24]Wang Feiyu, Jin Zhijun, Lü Xiuxiang,et al. Timing of petroleum accumulation: Theory and new methods [J]. Advances in Earth Science,2002,17(5):754-759.[王飞宇,金之钧,吕修祥,等.含油气盆地成藏期分析理论和新方法[J].地球科学进展，2002,17(5)：754-759.]
[25]Zhang Jun, Pang Xiongqi, Liu Luofu,et al. The distribution characteristics of silurian tar sand of Tarim bain and its petroleum geological significance [J].Science in China (Series D),2004,34（suppl.Ⅰ）:169-176.[张俊，庞雄奇，刘洛夫,等．塔里木盆地志留系沥青砂的分布特征与石油地质意义[J]．中国科学:D辑，2004，34（增刊 Ⅰ）：169-176.]
[26]Pang Xiongqi, Jiang Zhenxue, Zuo Shengjie. Study on destroyed hydrocarbon amount by tectonic event in superimposed basins[J].Geological Review,2002,48(4):384-390.[庞雄奇,姜振学，左胜杰.叠合盆地构造变动破坏烃量研究方法探讨[J].地质论评，2002,48(4)：384-390.]
[27]Pang Xiongqi, Zuo Shengjie, Jin Zhijun,et al. Inversion modeling of the hydrocarbon amount destroyed tectonic event in the Jiyang depression [J]. Petroleum Exploration and Development,2003,30(3):56-60.[庞雄奇,左胜杰,金之钧,等.济阳坳陷构造变动破坏烃量反演模拟[J].石油勘探与开发，2003,30(3)：56-60.]
[28]Luo Xiaorong. Review of hydrocarbon migration and accumulation dynamics [J].Natural Gas Geoscience,2003,14(5):337-346.[罗晓容.油气运聚动力学研究进展及存在问题[J].天然气地球科学，2003,14(5)：337-346.]
[29]Hou Ping, Zhou Bo, Luo Xiaorong. The model analysis on the second migration pathway of oil[J]. Science in China(Series D),2004, 34(suppl.Ⅰ):162-168.[侯平，周波，罗晓容.石油二次运移路径的模式分析[J].中国科学:D辑，2004, 34(增刊Ⅰ):162-168.]
[30]Davis R W. Analysis of hydrodynamic factors in petroleum migration and entrapment[J]. AAPG Bulletin,1987, 11(6)：643-649.
[31]Zhou Xingxi. The petroleum reservoir forming characteristics of the composite superimposed basin—An example from Tarim basin[J].Earth Science Frontiers,2000,7（3）:39-47.[周兴熙．复合叠合盆地油气成藏特征——以塔里木盆地为例[J]．地学前缘，2000，7（3）：39-47.]
[32]Dai Jinxing, Xia Xinyu, Hong Feng,et al. The main controlling factors for the formation of coal-formed big gas field in China[J].Chinese Science Bulletin,1999,44(22)：2 455-2 464.[戴金星，夏新宇，洪峰.中国煤成大中型气田形成的主要控制因素[J].科学通报，1999,44(22):2 455-2 464.]
[33]Dai Jinxing, Wei Yanzhao, Zhao Jingzhou. Important role of the formation of gas accumulation in the late stage in the formation of large gas fields[J]. Chinese Geology,2003,30（1）:10-19.[戴金星,卫延召，赵靖舟.晚期成藏对大气田形成的重大作用[J].中国地质，2003,30（1）：10-19.]
[34]Zhang Yiwei. Potentials and exploration prospect of China’s hydrocarbon resources[J].Petroleum Science，2004,1（1）：1-7.
[35]Bethke C M, Reed J D, Oltz D F. Long-range petroleum migration in the Illinois Basin[J].AAPG Bulletin,1991, 75(50)：925-945.
[36]Catalan L, Xiaowen F, Chatzis I,et al. An experimental study of secondary oil migration[J].AAPG Bulletin,1992, 76(5)：638-650.
[37]Zhou Xingxi.Essentials about hydrocarbon distribution controlled by source and seal[J].Petroleum Exploration and Development,1997,24(6):4-7.[周兴熙．源—盖共控论述要[J]．石油勘探与开发，1997，24(6):4-7.]
[38]Zhang Houfu, Zhang Wanxuan. Petroleum Geology（The second edition）[M]. Beijing: Petroleum Industry Press,1989.[张厚福，张万选，石油地质学（第2版）[M]．北京：石油工业出版社，1989.]

[1]	程有义. 含油气盆地二氧化碳成因研究[J]. 地球科学进展, 2000, 15(6): 684-687.

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