Advanced Search
Volume 32 Issue 6
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2010  >  32(6): 560-565
Shen Zhongmin, Jiang Min, Liu Sibing, Zhu Hongquan, Gong Yajun. PARTITION AND CONTRAST ON GENETIC TYPE OF CONTINENTAL NATURAL GAS IN THE SICHUAN BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(6): 560-565. doi: 10.11781/sysydz201006560
Citation: Shen Zhongmin, Jiang Min, Liu Sibing, Zhu Hongquan, Gong Yajun. PARTITION AND CONTRAST ON GENETIC TYPE OF CONTINENTAL NATURAL GAS IN THE SICHUAN BASIN[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(6): 560-565. doi: 10.11781/sysydz201006560
shu

PARTITION AND CONTRAST ON GENETIC TYPE OF CONTINENTAL NATURAL GAS IN THE SICHUAN BASIN

doi: 10.11781/sysydz201006560
  • 1.

    State Key Lab of Oil-gas Reservoirs Geology and Exploitation(Chengdu University of Technology), Chengdu, Sichuan 610059, China

  • 2. Exploration and Production Research Institute of Southwest Branch Company, SINOPEC, Chengdu, Sichuan 610081, China

  • 3. The Western New Research Center of Shengli Oilfield, SINOPEC, Dongying, Shandon 257000, China

  • Received Date: 2010-06-17
  • Rev Recd Date: 2010-10-27
  • Publish Date: 2010-12-28
    Abstract
  • The paper studies systematically the light hydrocarbon fingerprint, carbon isotope, hydrogen isotope and noble gas isotope of natural gas in the Sichuan Basin. The natural gas carbon isotope C1-C2 relationship from different areas and formations show that the natural gas in the Sichuan Basin were affected by parent types of sources rock, maturity, migration and other factors. The light hydrocarbon fingerprint indicates the major source of natural gas in the Western Sichuan Depression is humus-type, the sources in southern Sichuan Basin, eastern Sichuan Basin and the central region of Sichuan Basin are both humus-type and sapropel type, and the natural gas are mainly oil-type gas. The C1 isotope of natural gas from T3x2 in the middle area of the Western Sichuan Depression are higher than other areas and C2 isotope are less than -28‰, which shows oil-type gas and higher maturity feature. The natural gases of other formations in study area are concentrating distribution relatively and display the typical feature of coal-related gas. The marine and continental natural gas in the Sichuan Basin could be distinguished by carbon isotope δ13C2=-28‰ and hydrogen isotope δD1=-140‰ of the natural gas. The noble gas isotope shows that the natural gas are shell source without the addition of mantle noble gases.

     

    • FullText(HTML)
  • loading
    • References(50)
  • [1]
    张水昌,朱光有.四川盆地梅相天然气富集成藏特征与勘探潜力[J].石油学报,2006,27(5):1-8.
    [2]
    吴世祥,汤良杰.四川盆地碎屑岩领域有利天然气勘探方向浅析[J].西安石油大学学报(自然科学版),2006,21(1):20-57.
    [3]
    朱光有,张水昌,梁英波,等.四川盆地天然气特征及气源[J].地学前缘,2006,13(2):234-248.
    [4]
    沈忠民,潘中亮,吕正祥,等.川西坳陷中段须家河组天然气地球化学特征与气源追踪[J].成都理工大学学报(自然科学版),2009,36(3):225-230.
    [5]
    郑荣才,朱如凯,翟文亮,等.川西类前陆盆地晚三叠世须家河组构造演化及层序充填样式[J].中国地质,2008,35(2):246-255.
    [6]
    徐国盛,刘树根.川西前陆盆地碎屑岩天然气跨层运移过程中的相态演变[J].成都理工学院学报,2001,28(4):383-389.
    [7]
    KLUSMAN R W,VOORHEES K J,HICKEY J C,et al.A new approach to multi-component gas geochemistry in metal exploration[C].SEG,Exploration for ore deposits of the North American Cordillera,abstracts with program,1984:41.
    [8]
    戴金星.各类烷烃气的鉴别[J].中国科学B辑,1992(2):185-193.
    [9]
    HUNT J M.Generation and migration of light hydrocarbons[J].Science,1984,226:1265-1270.
    [10]
    黄志龙,高岗,刚文哲.川西平落坝气田原生与次生气藏烃类组成特征[J].天然气地球科学,2003,14(2):116-119.
    [11]
    钱志浩,曹寅,张美珍.川东北天然气单体烃氢同位素组成特征[J].海相油气地质,2008,13(2):17-21.
    [12]
    戴金星.我国有机烷烃气的氧同位素的若干特征[J].石油勘探与开发,1990,17(5):27-32.
    [13]
    戴金星,戚厚发,宋岩.鉴别煤成气和油型气若干指标的初步探讨[J].石油学报,1985,6(2):31-38.
    [14]
    戴金星.中国煤成气研究二十年的重大进展[J].石油勘探与开发,1999,26(3):1-9.
    [15]
    戴金星.天然气碳氢同位素特征和各类天然气鉴别[J].天然气地球科学,1993,4(2-3):1-40.
    [16]
    樊然学.川西坳陷中段气藏天然气形成、运移的碳同位素地球化学证据[J].自然科学进展,1999,9(12):11-26.
    [17]
    凡元芳.川东北地区普光气藏地球化学特征及成藏演化[D].武汉:中国地质大学,2006:40-43.
    [18]
    秦胜飞,陶上振,涂涛,等.川西坳陷天然气地球化学及成藏特征[J].石油勘探与开发,2007,34(1):34-38.
    [19]
    朱光有,张水昌,梁英波,等.四川盆地天然气特征及气源[J].地学前缘,2006,13(2):234-248.
    [20]
    黄籍中.再论四川盆地天然气地球化学特征[J].地球化学,1990(1):32-43.
    [21]
    王兰生,陈盛吉,杜敏,等.四川盆地三叠系天然气地球化学特征及资源潜力分析[J].天然气地球科学,2008,19(2):222-228.
    [22]
    杨家静,王一刚,王兰生,等.四川盆地东部长兴组-飞仙关组气藏地球化学特征及气源探讨[J].沉积学报,2002,20(2):349-352.
    [23]
    戴金星,夏新宇,卫延召,等.四川盆地天然气的碳同位素特征[J].石油实验地质,2001,23(2):115-132.
    [24]
    黄籍中,姜怀诚.四川盆地奥陶系天然气成因探讨[J].石油学报,1986,7(4):11-23.
    [25]
    王顺玉,戴鸿鸣,王海清,等.四川盆地海相碳酸盐岩大型气田天然气地球化学特征与气源[J].天然气地球科学,2000,11(2):10-17.
    [26]
    刘光祥,陶静源,潘文蕾,等.川东北及川东区天然气成因类型探讨[J].石油实验地质,2002,24(6):512-516.
    [27]
    谢增业,田世澄,李剑,等.川东北飞仙关组鲕滩天然气地球化学特征与成因[J].地球化学,2004,33(6):567-573.
    [28]
    王铜山.川东北飞仙关组鲕滩气藏天然气成因特征及其生成动力学研究[D].北京:中国科学院研究生院,2007:6-11.
    [29]
    肖芝华,谢增业,李志生,等.川中-川南地区须家河组天然气同位素组成特征[J].地球化学,2008.37(3):245-250.
    [30]
    李延钧,梁艳,雷卞军,等.川中-川南过渡带西部嘉二段天然气成因与来源[J].天然气地球科学,2006,17(6):820-823.
    [31]
    陈义才,郭贵安,蒋裕强,等.川中地区上三叠统天然气地球化学特征及成藏过程探讨[J].天然气地球科学,2007,18(5):737-742.
    [32]
    李弢,赵路子,陆正元,等.川南地区嘉陵江组天然气气源研究[J].天然气工业,2005,25(12):9-11.
    [33]
    秦胜飞,戴金星,王兰生.川西前陆盆地次生气藏天然气来源追踪[J].地球化学,2007,36(4):368-374.
    [34]
    樊然学,周洪忠,蔡开平.川西坳陷南段天然气来源与碳同位素地球化学研究[J].地球学报,2005,26(2):157-162.
    [35]
    徐永昌.天然气成因理论与应用[M].北京:科学出版社,1994:1-414.
    [36]
    王大锐.油气稳定同位素地球化学[M].北京:石油工业出版社,2000:214-217.
    [37]
    SCHOELL M.The hydrogen and carbon isotopic composition of methane from natural gases of various[J].Geochim Cosmochim Aeta,1980,44(5):649-661.
    [38]
    沈平,徐永昌.中国陆相成因天然气同位素特征[J].地球化学,1991(2):144-152.
    [39]
    沈平.天然气地球化学研究中的新认识和新发现[J].天然气地球科学,1990,1(1):37-38.
    [40]
    王晓锋,刘文汇,徐永昌,等.塔里木盆地天然气碳氢同位素地球化学特征[J].石油勘探与开发,2005,32(3):55-58.
    [41]
    HILKERT A W,DOUTHITT C B.Isotope ratio monitoringgas chromatography/mass spectrometry of D/H by high temperature conversion isotope ratio mass spectrometry[J].Rapid Communication in Mass Spectrometry,1999,13:1226-1230.
    [42]
    刘全有,戴金星,李剑,等.塔里木盆地天然气氢同位素地球化学与对热成熟度和沉积环境的指示意义[J].中国科学D辑:地球科学,2007,37(12):1599-1608.
    [43]
    陶成,把立强,王杰.天然气氢同位素分析及应用[J].石油实验地质,2008,30(1):94-97.
    [44]
    徐永昌,沈平,刘文汇,等.天然气中稀有气体地球化学研究[M].北京:科学出版社,1998:89-91.
    [45]
    戴金星,宋岩,戴春林,等.中国东部无机成因气及其气藏形成条件[M].北京:科学出版社,1995:212.
    [46]
    刘文汇,徐永昌.天然气中氦、氩同位素组成特征[J].科学通报,1993,38(9):818-821.
    [47]
    徐永昌.天然气中的幔源稀有气体[J].地学前缘,1996,3(3-4):63-70.
    [48]
    KANEOKA I,TAKAOKA N.Noble gas state in the Earth's interior[J].Chem Geol(Isotope Geoscience section),1985,52:75-95.
    [49]
    WAKITA H,SANO Y,URABEA,et al.Origin of methanerich natural gas in Japan:formation of gas fields due to largescale submarine volcanism[J].Applied Geochemistry,1990,5(3):263-278.
    [50]
    张晓宝,史朋,马素萍,等.应用稀有气体同位素判识油田水淹现象:以辽河盆地黄沙坨油田为例[J].石油实验地质,2009,1(3):258-261.
    • Relative Articles
    • Supplements(0)
    • Cited By
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索
    Citation
    XML
    PDF-CN

    Article Metrics

    Article views (3599) PDF downloads(871) Cited by()
    Proportional views
    Related

    Website Copyright © Wuxi Research Institute of Petroleum Geology, SINOPEC 苏ICP备15009037号 苏公网安备32021102000780号

    Address：No. 2060, Lihu Avenue, Wuxi, Jiangsu   (214126) Tel：0510-68787204，68787203 Fax：0510-68787113 Email：sysydz.syky@sinopec.com

    Supported by: Beijing Renhe Information Technology Co. Ltd    

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return