收稿日期: 2008-09-07
修回日期: 2008-12-18
网络出版日期: 2009-02-10
基金资助
国家重点基础研究发展计划项目(编号:113404GJ0003);国家自然科学基金项目(编号:40602016)联合资助.
Multiple Hydrocarbon Migration and Accumulation of TZ12 Structure, Tarim Basin
Received date: 2008-09-07
Revised date: 2008-12-18
Online published: 2009-02-10
武芳芳 朱光有 王慧 张水昌 金强 顾乔元 张宝收 苏劲 . 塔里木盆地塔中12构造复式油气运聚与成藏研究[J]. 天然气地球科学, 2009 , 20(1) : 76 -85 . DOI: 10.11764/j.issn.1672-1926.2009.01.76
TZ12 structure, an inherited paleo uplift during geologic epoch, is located in the central part of TZ10 structure. The show of oil and gas including fluorescence, oil slick, oil trace, asphalt and crude oil is quite active in many Silurian and Ordovician intervals. In addition, the industrial oil has been got in Silurian. The analysis reveals that the show of oil and gas, oil trace and fluorescence in Carboniferous may come from the underneath strata through fault leakage. The multiple oil/gas reservoiring process for Silurian and Upper Ordovician of TZ12 structure is discussed by analyzing fault seal, pyrrole nitrogen compound, source rock correlation as well as other scholars′ research on inclusion composition and homogenization temperature, which will help better understand the oil and gas distribution of Tazhong area. Moreover, the hydrocarbon pooling conditions of Lower Ordovician indicates that it′s quite likely to get industrial gas flow.
[1] 赵密福.断层封闭性研究现状[J].新疆石油地质,2004,25(3):333 -336.
[2] 付广,孟庆芬.断层封闭性影响因素的理论分析[J].天然气地球科学,2002,13(3 -4):40 -44.
[3] 刘琨,胡望水,陆建林.系统分析评价断层封闭能力的思路[J].石油勘探与开发,2004,31(2):87 -89.
[4] 何伟.断层封堵性的三级评价方法[J].油气地质与采收率,2005,12(2):23 -29.
[5] 李储华,刘启东,陈平原,等.高邮凹陷瓦庄东地区断层封闭性多方法对比研究[J].中国西部油气地质,2007,3(1):65 -68.
[6] 赵密福,李亚辉,信荃麟,等.鲁克沁构造带稠油成藏机制研究[J].石油大学学报,2001,25(1):51 -54.
[7] 付晓飞,孙永河,许凤明.胜利油区车古20潜山断层侧向封闭性研究[J].天然气工业,2006,26(7):32 -34.
[8] 吕延防,李国会,王跃文,等.断层封闭性的定量研究方法[J].石油学报,1996,17(3):39 -45.
[9] 刘洛夫,徐新德.含氮化合物与石油运移研究[J].勘探家,1996,1(2):33 -37.
[10] 霍红,刘洛夫,解启来,等.塔中地区志留系原油运移方向研究[J].新疆石油地质,2007,28(2):175 -178.
[11] 孙龙德,李曰俊,江同文,等.塔里木盆地塔中低凸起:一个典型的复式油气聚集区[J].地质科学,2007,42(3):602 -620.
[12] 张水昌,梁狄刚,张宝民,等.塔里木盆地海相油气的生成[M].北京:石油工业出版社,2004:30 -40.
[13] 张水昌,王飞宇,张宝民,等.塔里木盆地中上奥陶统油源地球化学研究[J].石油学报,2000,21(6):23 -28.
[14] 张水昌,张宝民,王飞宇,等.中—上奥陶统:塔里木盆地的主要油源层[J].海相油气地质,2000,5(1 -2):16 -22.
[15] 朱东亚,金之钧,胡文,等.塔中地区志留系砂岩中孔隙游离烃和包裹体烃对比研究及油源分析[J].石油与天然气地质,2007,28(1):25 -34.
[16] 张鼐,张水昌,李新景,等.塔中117井储层烃包裹体研究及油气成藏史[J].岩石学报,2005,21(5):1473 -1478.
[17] 吕修祥,解启来,杨宁,等.塔里木盆地深部流体改造型碳酸盐岩油气聚集[J].科学通报,2007,52(增刊I):142 -148.
[18] 赵雪凤,朱光有,刘钦甫,等.深部海相碳酸盐岩储层孔隙发育的主控因素研究[J].天然气地球科学,2007,18(4):514 -521.
[19] 朱光有,张水昌,梁英波,等.TSR对深部碳酸盐岩储层的溶蚀改造——四川盆地深部碳酸盐岩优质储层形成的重要方式[J].岩石学报,2006,22(8):2182 -2194.
[20] 张水昌,朱光有,梁英波.四川盆地普光大型气田H2S及优质储层形成机理探讨[J].地质论评,2006,52(2):230 -235.
[21] 朱光有,张水昌,马永生,等.TSR(H2S)对石油天然气工业的积极性研究——H2S的形成过程促进储层次生孔隙的发育[J].地学前缘,2006,13(3):141 -149.
[22] Zhu Guangyou,Zhang Shuichang,Liang Yingbo,et al.The genesis of H2S in the Weiyuan Gas Field,Sichuan Basin and its evidence[J].Chinese Science Bulletin,2007,52(10):1394 -1404.
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