Yang Keming. Hydrocarbon potential of source rocks in the Middle Triassic Leikoupo Formation in the Western Sichuan Depression[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2016, 38(3): 366-374. doi: 10.11781/sysydz201603366
Citation: Yang Keming. Hydrocarbon potential of source rocks in the Middle Triassic Leikoupo Formation in the Western Sichuan Depression[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2016, 38(3): 366-374. doi: 10.11781/sysydz201603366

Hydrocarbon potential of source rocks in the Middle Triassic Leikoupo Formation in the Western Sichuan Depression

doi: 10.11781/sysydz201603366
  • Received Date: 2016-01-26
  • Rev Recd Date: 2016-04-15
  • Publish Date: 2016-05-28
  • The Middle Triassic Leikoupo Formation in the Western Sichuan Depression is an important marine target for natural gas exploration in the Sichuan Basin in recent years. Geochemical analyses were made with rock samples from the Leikoupo Formation. Seismic interpretation and sedimentary data were studied. Source rocks in the Leikoupo Formation mainly distribute in Dayi, Wenjiang, Pengzhou, Guanghan and Xiaoquan. They are about 250-350 m thick, and have a TOC content of 0.4%-0.6%. The source rocks were deposited in a sedimentary environment with high biological productivity, quiescent depositional setting, restricted seawater circulation, high salinity, anoxic bottom water and low deposition rate, all favorable for the preservation of organic matter. The comprehensive analyses of organic geochemistry, inorganic geochemistry and organic petrology indicated that, the source rocks in the Leikoupo Formation displayed a low abundance of organic matter with good organic type. Solid bitumen and ultramicro macerals were observed on photomicrographs. Organic type index (TI) ranges from 12.5%-98.03%, indicating Type Ⅱ1-Ⅱ2 source rocks. Organic matter was mainly derived from hydroplankton, showing a good hydrocarbon potential.

     

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  • [1]
    郭正吾,邓康龄,韩永辉,等.四川盆地形成与演化[M].北京:地质出版社,1996. Guo Zhengwu,Deng Kangling,Han Yonghui,et al.The formation and development of Sichuan Basin[M].Beijing:Geological Publishing House,1996.
    [2]
    徐国盛,陈美玲,刘为,等.川西地区雷口坡组岩相古地理与富钾卤水预测[J].矿床地质,2012,31(2):309-322. Xu Guosheng,Chen Meiling,Liu Wei,et al.Lithofacies palaeogeography and forecast of potassium-rich brine of Leikoupo Formation in western Sichuan[J].Mineral Deposits,2012,31(2):309-322.
    [3]
    吕玉珍,倪超,张建勇,等.四川盆地中三叠统雷口坡组有利沉积相带及岩相古地理特征[J].海相油气地质,2013,18(1):26-32. Lü Yuzhen,Ni Chao,Zhang Jianyong,et al.Favorable sedimentary facies zones and lithofacies palaeogeography of Middle Triassic Lei-koupo Formation in Sichuan Basin[J].Marine Origin Petroleum Geology,2013,18(1):26-32.
    [4]
    吴世祥,李宏涛,龙胜祥,等.川西雷口坡组碳酸盐岩储层特征及成岩作用[J].石油与天然气地质,2011,32(4):542-550. Wu Shixiang,Li Hongtao,Long Shengxiang,et al.A study on characteristics and diagenesis of carbonate reservoirs in the Middle Triassic Leikoupo Formation in Western Sichuan Depression[J].Oil & Gas Geology,2011,32(4):542-550.
    [5]
    唐宇.川西地区雷口坡组沉积与其顶部风化壳储层特征[J].石油与天然气地质,2013,34(1):42-47. Tang Yu.Characterization of the sedimentation of the Leikoupo Formation and the weathering crust reservoirs at the top of the formation in the western Sichuan Basin[J].Oil & Gas Geology,2013,34(1):42-47.
    [6]
    宋晓波,王琼仙,隆轲,等.川西地区中三叠统雷口坡组古岩溶储层特征及发育主控因素[J].海相油气地质,2013,18(2):8-14. Song Xiaobo,Wang Qiongxian,Long Ke,et al.Characteristics and main controlling factors of Middle Triassic Leikoupo paleokarst reservoirs in western Sichuan Basin[J].Marine Origin Petroleum Geology,2013,18(2):8-14.
    [7]
    张永刚,马宗晋,杨克明,等.川西坳陷中段海相层系油气勘探潜力分析[J].地质学报,2007,81(8):1041-1047. Zhang Yonggang,Ma Zongjin,Yang Keming,et al.The forecast of natural oil & gas potential in marine strata,western Sichuan Basin,Southwest China[J].Acta Geologica Sinica,2007,81(8):1041-1047.
    [8]
    许国明,宋晓波,王琼仙.川西坳陷中段三叠系雷口坡组-马鞍塘组油气地质条件及有利勘探目标分析[J].海相油气地质,2012,17(2):14-19. Xu Guoming,Song Xiaobo,Wang Qiongxian.Analysis of petroleum geologic conditions and favorable prospecting targets of Triassic Leikoupo-Ma' antang formations in the middle segment of Chuanxi Depression,western Sichuan Basin[J].Marine Origin Petroleum Geology,2012,17(2):14-19.
    [9]
    谢刚平.川西坳陷中三叠统雷口坡组四段气藏气源分析[J].石油实验地质,2015,37(4):418-422,429. Xie Gangping.Source of gas reservoirs in the fourth member of the Middle Triassic Leikoupo Formation in Western Sichuan Depression[J].Petroleum Geology & Experiment,2015,37(4):418-422,429.
    [10]
    廖凤蓉,吴小奇,黄士鹏,等.川西北地区中坝气田雷口坡组天然气地球化学特征及气源探讨[J].天然气地球科学,2013,24(1):108-115. Liao Fengrong,Wu Xiaoqi,Huang Shipeng,et al.Geochemical cha-racteristics and gas-source correlation of Leikoupo Formation in Zhongba Field,Northwest Sichuan Basin[J].Natural Gas Geoscience,2013,24(1):108-115.
    [11]
    腾格尔,秦建中,付小东,等.川西北地区海相油气成藏物质基础:优质烃源岩[J].石油实验地质,2008,30(5):478-483. Tenger,Qin Jianzhong,Fu Xiaodong,et al.Basic conditions of marine hydrocarbon accumulation in Northwest Sichuan Basin:High guality source rocks[J].Petroleum Geology & Experiment,2008,30(5):478-483.
    [12]
    秦建中.中国烃源岩[M].北京:科学出版社,2005. Qin Jianzhong.Source rocks in China[M].Beijing:Science Press,2005.
    [13]
    卢龙飞.海相烃源中有机-矿物相互作用及有机质演化[R].无锡:中国石化无锡石油地质研究所,2012:1-98. Lu Longfei.Interaction between organic matters and minerals and organic matter evolution in marine source rocks[R].Wuxi:Wuxi Institute of Petroleum Geology,SINOPEC,2012:1-98.
    [14]
    梁狄刚,张水昌,张宝民,等.从塔里木盆地看中国海相生油问题[J].地学前缘,2000,7(4):534-547. Liang Digang,Zhang Shuichang,Zhang Baomin,et al.Understanding on marine oil generation in China based on Tarim Basin[J].Earth Science Frontiers,2000,7(4):534-547.
    [15]
    赵振华.微量元素地球化学原理[M].北京:科学出版社,1997:56-206. Zhao Zhenhua.Geochemical principles of trace elements[M].Beijing:Science Press,1997:56-206.
    [16]
    Passier H F,Bosch H J,Nijenhuis I A,et al.Sulphidic Mediterranean surface waters during Pliocene sapropel formation[J].Nature,1999,397(6715):146-149.
    [17]
    叶连俊.生物有机质成矿作用和成矿背景[M].北京:海洋出版社,1998:335-352. Ye Lianjun.Metallogeny and metallogenic background of bio-organic matters[M].Beijing:China Ocean Press,1998:335-352.
    [18]
    腾格尔,刘文汇,徐永昌,等.海相地层无机参数与烃源岩发育环境的相关研究:以鄂尔多斯盆地为例[J].石油与天然气地质,2005,26(4):411-421. Tenger,Liu Wenhui,Xu Yongchang,et al.Study on relation between inorganic parameters in marine deposits and developmental environment of hydrocarbon source rocks:Taking Ordos Basin as an example[J].Oil & Gas Geology,2005,26(4):411-421.
    [19]
    郑永飞,陈江峰.稳定同位素地球化学[M].北京:科学出版社,2000:203-218. Zheng Yongfei,Chen Jiangfeng.Stable isotope geochemistry[M].Beijing:Science Press,2000:203-218.
    [20]
    王大锐,白玉雷,贾承造.塔里木盆地油区石炭系海相碳酸盐岩同位素地球化学研究[J].石油勘探与开发,2001,28(6):38-41. Wang Darui,Bai Yulei,Jia Chengzao.Stable isotopic geochemistry of the Carboniferous marine carbonates in the Tarim Basin[J].Petroleum Exploration and Development,2001,28(6):38-41.
    [21]
    Kump L R,Arthur M A.Interpreting carbon-isotope excursions:Carbonates and organic matter[J].Chemical Geology,1999,161(1/3):181-198.
    [22]
    加里莫夫Э M.生物圈碳同位素组成全球变化特点[J].李红光,译.天然气地球化学,2002,13(1/2):1-17. Galimov E M.Global changes of carbon isotope composition in biosphere[J].Li Hongguang,trans.Natural Gas Geoscience,2002,13(1/2):1-17.
    [23]
    杨瑞东,王世杰,欧阳自远,等.元古宙-寒武纪疑源类的辐射演化、绝灭作用与海洋地球化学演变:兼论扬子区元古宙-奥陶纪疑源类的演化[J].地质地球化学,2001,29(4):65-72. Yang Ruidong,Wang Shijie,Ouyang Ziyuan,et al.Study on the relationship between radiation and extinction of Proterozoic and Cambrian phytoplanktons (acritarchs) and marine geochemical evolution[J].Geology-Geochemistry,2001,29(4):65-72.
    [24]
    Hunt J M.Petroleum geochemistry and geology[M].New York:Freeman,1979:62-273.
    [25]
    颜佳新,徐四平,李方林.湖北巴东栖霞组缺氧沉积环境的地球化学特征[J].岩相古地理,1998,18(6):27-32. Yan Jiaxin,Xu Siping,Li Fanglin.Geochemistry of the dysaerobic sedimentary environments of the Qixia Formation in Badong,Hubei[J].Sedimentary Facies and Palaeogeography,1998,18(6):27-32.
    [26]
    李任伟.蒸发盐环境沉积岩有机质和生油研究[M].北京:海洋出版社,1993:19-22. Li Renwei.Organic matters in sediments and their hydrocarbon generation potential under evaporation salt environment[M].Beijing:China Ocean Press,1993:19-22.
    [27]
    游海涛,程日辉,刘昌岭.古盐度复原法综述[J].世界地质,2002,21(2):111-117. You Haitao,Cheng Rihui,Liu Changling.Review of paleosalinity recovering methods[J].World Geology,2002,21(2):111-117.
    [28]
    陈荣坤.稳定氧碳同位素在碳酸盐岩成岩环境研究中的应用[J].沉积学报,1994,12(4):11-21. Chen Rongkun.Application of stable oxygen and carbon isotope in the research of carbonate diagenetic environment[J].Acta Sedimentologica Sinica,1994,12(4):11-21.
    [29]
    腾格尔,刘文汇,徐永昌,等.高演化海相碳酸盐烃源岩地球化学综合判识:以鄂尔多斯盆地为例[J].中国科学(D辑地球科学),2006,36(2):167-176. Tenger,Liu Wenhui,Xu Yongchang,et al.Comprehensive geochemical identification of highly evolved marine carbonate rocks as hydrocarbon-source rocks as exemplified by the Ordos Basin[J].Science in China (Series D Earth Sciense),2006, 49(4):384-396.
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