天然气地球科学

• 天然气地球化学 • 上一篇    下一篇

中上扬子地区二叠系烃源岩特征

罗进雄,何幼斌   

  1. 1.长江大学地球科学学院,湖北  武汉 430100;2.长江大学油气资源与勘探技术教育部重点实验室,湖北  武汉 430100
  • 收稿日期:2013-10-22 修回日期:2014-03-31 出版日期:2014-09-10 发布日期:2014-09-10
  • 通讯作者: 何幼斌(1964-),男,湖北黄冈人,教授,博士,博士生导师,主要从事沉积学教学和研究工作. E-mail:heyoubin@yangtzeu.edu.cn.
  • 作者简介:罗进雄(1980-),男,湖北天门人,副教授,博士,主要从事沉积学教学和研究工作. E-mail:luojinxiong1980@126.com.
  • 基金资助:
    国家自然科学基金项目“中上扬子地区中二叠世缺氧环境成因模式研究”(编号:41402089);国家科技重大专项项目“中上扬子海相碳酸盐岩成藏条件与有利勘探区带评价研究”(编号:2011ZX05004-001-004)联合资助.
     

Characteristics of the Permian Source Rocks in the Middle and Upper Yangtze Region

LUO Jin-xiong,HE You-bin   

  1.  

    (1.School of Geosciences,Yangtze University,Wuhan 430100,China;
    2.Key Laboratory of Exploration Technologies for Oil and Gas Resources,Ministry of Education,Yangtze University,Wuhan 430100,China)
  • Received:2013-10-22 Revised:2014-03-31 Online:2014-09-10 Published:2014-09-10

摘要:

基于烃源岩的类型、分布,有机质的丰度、成熟度等方面的分析,对中上扬子地区二叠系烃源岩的特征进行了详细研究,并对烃源岩发育的控制因素进行了探讨。研究表明:中上扬子地区二叠系烃源岩主要为暗色碳酸盐岩、暗色泥(页)岩和煤,薄层硅岩也是潜在的烃源岩;其中中二叠统烃源岩以暗色碳酸盐岩为主,上二叠统烃源岩以暗色碳酸盐岩和暗色泥(页)岩为主;栖霞阶和茅口阶烃源岩厚度较大,分布较广;吴家坪阶和长兴阶烃源岩厚度相对较小,分布相对较局限;川西北—川东北—渝东—鄂西—黔北—黔中地区是各阶烃源岩分布的叠合区,是有利的生烃区带;研究区二叠系烃源岩的发育与沉积环境和上升流作用的关系密切,沉积环境控制着烃源岩的岩石类型和有机质丰度,中二叠统优质烃源岩的发育还与上升流的作用有关。
 

关键词: 中上扬子地区, 二叠系, 烃源岩, 沉积环境, 上升流

Abstract:

Based on the analysis of the types and distribution of source rocks and the abundance and maturity of organic matter,the characteristics of the Permian source rocks in the Middle and Upper Yangtze Region were studied in detail,and the controlling factors of the development of the source rocks were discussed.The results show that the Permian source rocks in study area are mainly composed of dark carbonate rocks,dark mudstones or shale and coal,and the thin-bedded siliceous rocks are also potential source rocks.The thickness of the source rocks of the Qixia Stage and the Maokou Stage is rather thick with wide distribution,and the thickness of the source rocks of the Wujiaping Stage and the Changxing Stage is relatively thin with rather limited distribution| and the area of northwestern Sichuan-northeastern Sichuan-eastern Chongqing-western Hubei-northern Guozhou-central Guizhou is the superimposed area of source rocks of the four stages,where is the favorable hydrocarbon zone.The development of the source rocks of the Permian in the study area is controlled by the sedimentary environment and the action of the upwelling.The types of source rocks and abundance of organic matter are mainly controlled by the sedimentary environments| and the development of the high-quality source rocks of the Middle Permian is closely related to the upwelling.
 
 

Key words: Middle and Upper Yangtze Region, Permian, Source rocks, Sedimentary environment, Upwelling

中图分类号: 

  • TE122.1+13
[1]Guo Xusheng,Hu Dongfeng.Newest progress and key techniques in gas exploration of reef-bank reservoir in the northern Sichuan Basin[J].Natural Gas Industry,2011,31(10):6-11.[郭旭升,胡东风.川东北礁滩天然气勘探新进展及关键技术[J].天然气工业,2011,31(10):6-11.]
[2]Guo Tonglou.Basic characteristics of deep reef-bank reservoirs and major controlling factors of gas pools in the Yuanba Gasfield[J].Natural Gas Industry,2011,31(10):12-16.[郭彤楼.元坝深层礁滩气田基本特征与成藏主控因素[J].天然气工业,2011,31(10):12-16.]
[3]Feng Zengzhao,Li Shangwu,Yang Yuqing,et al.Potential of oil and gas of the Permian of south China from the viewpoint of lithofacies palaeogeography[J].Acta Petrolei Sinica,1997,18(1):10-17.[冯增昭,李尚武,杨玉卿,等.从岩相古地理论中国南方二叠系油气潜景[J].石油学报,1997,18(1):10-17.]
[4]Ma Yongsheng.Geochemical characteristics and origin of natural gases from Puguang Gasfield on eastern Sichuan Basin[J].Natural Gas Geoscience,2008,19(1):1-7.[马永生.普光气田天然气地球化学特征及气源探讨[J].天然气地球科学,2008,19(1):1-7.]
[5]Chen Dan.Difference analysis of Changxing Formation gas reservoir between Puguang Gasfield and Yuanba Gasfield in the northeast of Sichuan area[J].Journal of Oil and Gas,2011,33(10):11-14.[陈丹.川东北地区元坝气田与普光气田长兴组气藏特征对比分析[J].石油天然气学报,2011,33(10):11-14.]
[6]Cai Liguo.Problems and suggestions on marine petroleum exploration on south China[J].Petroleum Geology and Experiment,2003,25(6):634-636.[蔡立国.中国南方海相油气勘探主要研究方向[J].石油实验地质,2003,25(6):634-636.]
[7]Dou Lirong,Wang Yigang.Formation and distribution of the Paleozoic marine carbonate rock of the pools in China[J].Petroleum Geology and Experiment,2003,25(5):419-425.[窦立荣,王一刚.中国古生界海相碳酸盐岩油气藏的形成与分布[J].石油实验地质,2003,25(5):419-425.]
[8]Cai Xunyu,Wei Baodong,Zhao Peirong.Characteristics of the marine hydrocarbon sources in south China[J].Natural Gas Industry,2005,25(3):20-22.[蔡勋育,韦宝东,赵培荣.南方海相烃源岩特征分析[J].天然气工业,2005,25(3):20-22.]
[9]Liu Guangxiang.Characteristics of Middle Palaeozoic marine source rock in the north margin of Middle and Upper Yangtze Region[J].Petroleum Geology and Experiment,2005,27(5):490-495.[刘光祥.中上扬子北缘中古生界海相烃源岩特征[J].石油实验地质,2005,27(5):490-495.]
[10]Xiao Kaihua,Wo Yujin,Zhou Yan,et al.Petroleum reservoiring characteristics and exploration direction in marine strata in southern China[J].Oil and Gas Geology,2006,27(3):316-325.[肖开华,沃玉进,周雁,等.中国南方海相层系油气成藏特点与勘探方向[J].石油与天然气地质,2006,27(3):316-325.]
[11]Chen Hongde,Pang Lin,Ni Xinfeng,et al.New brief remarks on hydrocarbon prospecting of marine strata in the Middle and Upper Yangtze Region[J].Petroleum Geology and Experiment,2007,29(1):13-18.[陈洪德,庞林,倪新峰,等.中上扬子地区海相油气勘探前景[J].石油实验地质,2007,29(1):13-18.]
[12]Chen Shengji,Xie Banghua,Wan Maoxia,et al.Source rock and resource potential of reef and shoal gas reservoirs in Sichuan Basin[J].Natural Gas Exploration and Development,2007,30(4):1-14.[陈盛吉,谢邦华,万茂霞,等.川北地区礁、滩气藏的烃源岩条件与资源潜力分析[J].天然气勘探与开发,2007,30(4):1-14.]
[13]Huang Darui,Cai Zhongxian,Zhu Yangming.The sedimentary setting and the source rock of Longtan(Wujiaping) strata in the northeastern Sichuan Basin[J].Offshore Oil,2007,27(3):57-63.[黄大瑞,蔡忠贤,朱扬明.川东北龙潭(吴家坪)组沉积相与烃源岩发育[J].海洋石油,2007,27(3):57-63.]
[14]Liang Digang,Guo Tonglou,Chen Jianping,et al.Distribution of four suits of regional marine source rocks[J].Marine Origin Petroleum Geology,2008,13(2):1-16.[梁狄刚,郭彤楼,陈建平,等.南方四套区域海相烃源岩的分布[J].海相油气地质,2008,13(2):1-16.]
[15]Dai Jinxing,Qin Shengfei,Tao Shizhen,et al.Developing trends of natural gas industry and the significant progress on natural gas geological theories in China[J].Natural Gas Geoscience,2005,16(2):127-142.[戴金星,秦胜飞,陶士振,等.中国天然气工业发展趋势和天然气地学理论重要进展[J].天然气地球科学,2005,16(2):127-142.]
[16]Jin Zhijun,Cai Liguo.Inheritance and innovation of marine petroleum geological theory in China[J].Acta Geologica Sinica,2007,81(8):1017-1024.[金之钧,蔡立国.中国海相层系油气地质理论的继承与创新[J].地质学报,2007,81(8):1017-1024.]
[17]Ma Li,Chen Huanjiang,Gan Kewen,et al.Tectonic and Marine Petroleum Geology of South China:Volume 1[M].Beijing:Geological Publishing House,2004:3-8.[马力,陈焕疆,甘克文,等.中国南方大地构造和海相油气地质(上)[M].北京:地质出版社,2004:3-8.]
[18]Zeng Dingqian.A memory of Permian in Huaying-Shan,Sichuan province[J].Bulletin of the Chinese Academy of Geological Science,1984,5(9):109-117.[曾鼎乾.四川华蓥山二叠系调查追记[J].中国地质科学院院报,1984,5(9):109-117.]
[19]Zhang Zhenghua.Permian Stratigraphy of Northern Guizhou[M].Guiyang:Guizhou People′s Publishing House,1988:1-113.[张正华.黔南二叠纪地层[M].贵阳:贵州人民出版社,1988:1-113.]
[20]Sheng Jinzhang,Jin Yugan.Correlation of Permian Deposits in China[M].Nanjing:Nanjing University Press,1994:14-113.
[21]Jin Yugan,Wang Shanghua,Shang Qinghua,et al.Chronostratigraphic subdivision and correlation of the Permian in China[J].Acta Geologica Sinica,1999,73(2):97-108.[金玉玕,王向东,尚庆华,等.中国二叠纪年代地层划分和对比[J].地质学报,1999,73(2):97-108.]
[22]Editorial Board of Stratigraphical Lexicon of China.Stratigraphical Lexicon of China Permian[M].Beijing:Geological Publishing House,2000:1-119.[中国地层典编委会.中国地层典——二叠系[M].北京:地质出版社,2000:1-119.]
[23]Li Guohui,Li Xiang,Song Shuyun,et al.Dividing Permian into 3 series and its significance in Sichuan Basin[J].Natural Gas Exploration & Development,2005,28(3):98-103.[李国辉,李翔,宋蜀筠,等.四川盆地二叠系三分及其意义[J].天然气勘探与开发,2005,28(3):20-26.]
[24]Feng Zengzhao,Yang Yuqing,Jin Zhenkui,et al.Lithofacies paleogeography of Permian South China[M].Dongying:Publishing House of University of Petroleum,1997:1-140.[冯增昭,杨玉卿,金振奎,等.中国南方二叠纪岩相古地理[M].东营:石油大学出版社,1997:1-140.]
[25]Luo Jinxiong,He Youbin.Origin and characteristics of Permian eyeball-shaped limestones in Middle-Upper Yangtze Region[J].Geological Review,2010,56(5):629-637.[罗进雄,何幼斌.中—上扬子地区二叠系眼球状石灰岩特征及成因研究[J].地质论评,2010,56(5):629-637.]
[26]Luo Jinxiong,He Youbin.Anoxic environments of the Permian of Middle and Upper Yangtze Area[J].Journal of Palaeogeography,2011,13(1):11-20.[罗进雄,何幼斌.中上扬子地区二叠纪缺氧环境[J].古地理学报,2011,13(1):11-20.]
[27]Li Hongjing.Sequence Stratigraphy Analysis and High Quality Source Rock Identification in Typical Permian Sections,Yangtze Area[D].Wuhan:China University of Geosciences,2009:73-87.[李红敬.扬子地区二叠系典型剖面层序地层分析及优质烃源岩判识[D].武汉:中国地质大学,2009:73-87.]
[28]Li Hongjing,Xie Xinong,Lin Zhengliang,et al.Organic matter enrichment of Dalong Formation in Guangyuan area of the Sichuan Basin[J].Geological Science and Technology Information,2009,28(2):98-103.[李红敬,解习农,林正良,等.四川盆地广元地区大隆组有机质富集规律[J].地质科技情报,2009,28(2):98-103.]
[29]Tenger,Qin Jianzhong,Fu Xiaodong,et al.Hydrocarbon source rocks evaluation of the Upper Permian Wujiaping Formation in northeastern Sichuan area[J].Journal of Palaeogeography,2010,12(3):334-345.[腾格尔,秦建中,付小东,等.川东北地区上二叠统吴家坪组烃源岩评价[J].古地理学报,2010,12(3):334-345.]
[30]Harry D.Three common source rock evaluation errors made by geologists during prospect or play appraisals[J].AAPG Bulletin,2009,93(3):341-356.
[31]Cai Kaiping,Wang Yingrong,Yang Yueming,et al.Evaluation of hydrocarbon source rocks in Permian and Triassic at Guangyuan-Wangcang region in northwest Sichuan Basin and a primary discussion on gas source[J].Natural Gas Industry,2003,23(2):10-14.[蔡开平,王应蓉,杨跃明,等.川西北广旺地区二、三叠系烃源岩评价及气源初探[J].天然气工业,2003,23(2):10-14.]
[32]Wang Lansheng,Li Zirong,Xie Yaoxiang,et al.Research on minimum TOC of source rock of Permian carbonate in southwest Sichuan Basin[J].Natural Gas Geoscience,2003,14(1):39-46.[王兰生,李子荣,谢姚祥,等.川西南地区二叠系碳酸盐岩生烃下限研究[J].天然气地球科学,2003,14(1):39-46.]
[33]Lin Xiaoyun,Liu Jian.Application of the mechanism of hydrocarbon regeneration to evaluation of source rocks of high maturity in Middle and Lower Yangtze Region[J].Marine Geology and Quaternary Geology,2007,27(5):99-104.[林小云,刘建.二次生烃机理在中下扬子高演化烃源岩评价中的应用[J].海洋地质与第四纪地质,2007,27(5):99-104.]
[34]Fu Xiaodong,Qin Jianzhong,Tenger.Evaluation on excellent marine hydrocarbon source layers in southeast area of the Sichuan Basin:An example from well D-1[J].Petroleum Geology and Experiment,2008,30(6):621-628.[付小东,秦建中,腾格尔.四川盆地东南部海相层系优质烃源岩评价——以丁山1井为例[J].石油实验地质,2008,30(6):621-628.]
[35]Qin Jianzhong,Fu Xiaodong,Tenger.Evaluation of the excellent Triassic to Silurian marine hydrocarbon source rocks in Xuanhan-Daxian area of northeast Sichuan Basin[J].Petroleum Geology and Experiment,2008,30(4):367-374.[秦建中,付小东,腾格尔.川东北宣汉—达县三叠—志留系海相优质烃源层评价[J].石油实验地质,2008,30(4):367-374.]
[36]Xu Shenglin,Chen Hongde,Chen Anqing,et al.Source rock characteristics of marine strata,Sichuan Basin[J].Journal of Jilin University:Earth Science Edition,2011,41(2):343-350.[徐胜林,陈洪德,陈安清,等.四川盆地海相地层烃源岩特征[J].吉林大学学报:地球科学版,2011,41(2):343-350.]
[37]Lü Bingquan.Introduction to Marine Geology[M].Shanghai:Tongji University Press,2008:233-246.[吕炳全.海洋地质学概论[M].上海:同济大学出版社,2008:233-246.]
[38]Lü Bingquan,Hu Wangshui,Wang Honggang,et al.Neoproterozoic-Mesoproterozoic upwelling facies and its relationship with hydrocarbon in north China[J].Marine Geology and Quaternary Geology,2005,25(3):83-88.[吕炳全,胡望水,王红罡,等.华北地块中—上元古界上升流沉积相及其与油气的关系[J].海洋地质与第四纪地质,2005,25(3):83-88.]
 
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