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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2014  >  36(1): 95-101
Peng Jinning, Zhang Min, Liu Guangxiang, Pan Wenlei. Sedimentary environments and controlling factors of Permian source rocks in northeastern Sichuan Basin：A case study of Muguakou profile in Chengkou[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(1): 95-101. doi: 10.11781/sysydz201401095
Citation: Peng Jinning, Zhang Min, Liu Guangxiang, Pan Wenlei. Sedimentary environments and controlling factors of Permian source rocks in northeastern Sichuan Basin：A case study of Muguakou profile in Chengkou[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(1): 95-101. doi: 10.11781/sysydz201401095
shu

Sedimentary environments and controlling factors of Permian source rocks in northeastern Sichuan Basin：A case study of Muguakou profile in Chengkou

doi: 10.11781/sysydz201401095
  • 1.

    Department of Geochemistry, Yangtze University, Wuhan, Hubei 430100

  • 2. Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China

  • Received Date: 2013-05-20
  • Rev Recd Date: 2014-01-06
  • Publish Date: 2014-01-28
    Abstract
  • Based on previous analyses as well as filed outcrop observations and sample tests, a case study of the Permian profile in the Chengkou area of the northeastern Sichuan Basin was carried out. Palaeoenvironment was restored according to the parameters of macroelement (oxidizing material) and microelement, and the relationship between palaeoenvironment and source rock development was analyzed. The controlling factors for the vertical and horizontal distributions of source rock were discussed. Several conclusions were made as followed. 1) On plane map, the source rocks of deepwater marine shelf and interplatform basin facies had the highest organic matter abundance and were most widespread in Permian in the study area. The source rocks of innerplatform depression subfacies had lower organic matter abundance. 2) Vertically, the Permian source rocks mainly developed in transgressive hemicycle, and reached the highest organic matter abundance during the maximum flooding period. 3) Organic matter abundance was controlled by ancient biological productivity and organic matter preservation condition. Both of the 2 factors were necessary for high organic matter abundance.

     

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    • References(20)
  • [1]
    吴群, 彭金宁.川东北地区埋藏史及热史分析:以普光2井为例[J].石油实验地质, 2013, 35(2):133-138. Wu Qun, Peng Jinning.Burial and thermal histories of northeastern Sichuan Basin:a case study of well Puguang 2[J].Petroleum Geology & Experiment, 2013, 35(2):133-138.
    [2]
    Demaison G J, Moor G T.Anoxic environments and oil source bed genesis[J].AAPG Bulletin, 1980, 64(8):1179-1209.
    [3]
    Hunt J M.Petroleum geochemistry and geology[M].New York:Freeman, 1979:62-273.
    [4]
    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.
    [5]
    Chester R.Marine geochemistry[M].London:Blackwell Publishing, 2000:373-378.
    [6]
    Alberdi-Genolet M, Tocco R.Trace metals and organic geochemistry of the Machiques Member (Aptian-Albian) and La Luna Formation (Cenomanian-Campanian), Venezuela[J].Chemical Geology, 1999, 160(1-2):19-38.
    [7]
    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.The principle of microelement geochemistry[M].Beijing:Science Press, 1997:56-206.
    [8]
    加里莫夫E 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. Garymerv E M.The global changing characristics of carbon isotope in biosphere[J].Li Hongguang, tranlation, Natural Gas Geochemistry, 2002, 13(1-2):1-17.
    [9]
    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. Zhen Yongfei, Chen Jiangfeng.Stable isotope geochemistry[M].Beijing:Science Press, 2000:203-218.
    [10]
    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, LiuWenhui, 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.
    [11]
    刘全有, 金之钧, 高波, 等.四川盆地二叠系烃源岩类型与生烃潜力[J].石油与天然气地质, 2012, 22(1):10-18. Liu Quanyou, Jin Zhijun, Gao Bo, et al.Types and hydrocarbon generation potential of the Permian source rocks in the Sichuan Basin[J].Oil & Gas Geology, 2012, 22(1):10-18.
    [12]
    赵宗举, 周惠, 陈轩, 等.四川盆地及邻区二叠纪层序岩相古地理及有利勘探区带[J].石油学报, 2012, 33(S2):35-51. Zhao Zongju, Zhou Hui, Chen Xuan, et al.Sequence lithofacies paleogeography and favorable exploration zones of the Permian in Sichuan Basin and adjacent areas, China[J].Acta Petrolei Sinica, 2012, 33(S2):35-51.
    [13]
    王春梅, 王春连, 刘成林, 等.四川盆地东北部长兴期沉积相、沉积模式及其演化[J].中国地质, 2011, 38(3):594-609. Wang Chunmei, Wang Chunlian, Liu Chenglin, et al.Sedimentary facies, sedimentary model and evolution of Changxing Formation in northeast Sichuan basin[J].Chinese Geology, 2011, 38(3):594-609.
    [14]
    田成伟, 安显银, 罗清园, 等.川东北元坝地区长兴组层序地层及沉积相分析[J].地球科学与环境学报, 2012, 34(4):36-42. Tian Chengwei, An Xianyin, Luo Qingyuan, et al.Analysis of Sequence Stratigraphy and Sedimentary Facies of Changxing Formation in Yuanba Area of Northeast Sichuan[J].Journal of Earth Sciences and Environment, 2012, 34(4):36-42.
    [15]
    赵俊兴, 李凤杰, 刘琪, 等.四川盆地东北部二叠系沉积相及其演化分析[J].天然气地球科学, 2008, 19(4):444-452. Zhao Junxing, Li Fengjie, Liu Qi, et al.Analysis on permian sedimentary facies and its lithofacies palaeogeographic evolution, Northeast Sichuan Basin[J].Natural Gas Geoscience, 2008, 19(4):444-452.
    [16]
    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 disgenetic environment[J].Acta Sedimentologica Sinica, 1994, 12(4):11-21.
    [17]
    胡明毅, 魏国齐, 胡忠贵, 等.四川盆地中二叠统栖霞组层序:岩相古地理[J].古地理学报, 2010, 12(5):515-526. Hu Mingyi, Wei Guoqi, Hu Zhonggui, et al.Sequence-lithofacies palaeogeography of the Middle Permian Qixia Formation in Sichuan Basin[J].Journal of Palaeogeography, 2010, 12(5):515-526.
    [18]
    田雨, 张兴阳, 何幼斌, 等.四川盆地晚二叠世吴家坪期岩相古地理[J].古地理学报, 2010, 12(2):164-176. Tian Yu, Zhang Xingyang, He Youbin, et al.Lithofacies palaeogeography of the Late Permian Wujiaping Age of Sichuan Basin[J].Journal of Palaeogeography, 2010, 12(2):164-176.
    [19]
    Mazumdar A, Banerjee D M, Schidlowski M, et al.Rare-earth elements and stable isotope geochemistry of early Cambrian chert-phosphorite assemblages from the Lower Tal Formation of the Krol Belt (Lesser Himalaya, India)[J].Chemical Geology, 1999, 156(1-4):275-297.
    [20]
    陈建芳.古海洋研究中的地球化学新指标[J].地球科学进展, 2002, 17(3):402-409. Chen Jianfang.New geochemical Proxies in paleoc-eanography studies[J].Advances in Earth Sciences, 2002, 17(3):402-409.
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