Advanced Search
Volume 32 Issue 3
. 
Turn off MathJax
Article Contents
Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2010  >  32(3): 276-281
Wang Licheng, Wang Chengshan, Wu Xinhe, Li Yalin, Wei Yushuai. EVALUATION OF JURASSIC-CRETACEOUS MARINE HYDROCARBON ROCKS IN THE BOLIN BASIN, SOUTHWESTERN TIBET[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(3): 276-281. doi: 10.11781/sysydz201003276
Citation: Wang Licheng, Wang Chengshan, Wu Xinhe, Li Yalin, Wei Yushuai. EVALUATION OF JURASSIC-CRETACEOUS MARINE HYDROCARBON ROCKS IN THE BOLIN BASIN, SOUTHWESTERN TIBET[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2010, 32(3): 276-281. doi: 10.11781/sysydz201003276
shu

EVALUATION OF JURASSIC-CRETACEOUS MARINE HYDROCARBON ROCKS IN THE BOLIN BASIN, SOUTHWESTERN TIBET

doi: 10.11781/sysydz201003276
  • 1.

    School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

  • 2. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China

  • 3. SINOPEC Exploration and Production Research Institute, Beijing 100083, China

  • 4. Tibet Institutes of Geological Survey, Lhasa 850000, China

  • Received Date: 2009-11-11
  • Rev Recd Date: 2010-03-29
  • Publish Date: 2010-06-28
    Abstract
  • The Bolin Basin,located on the southwestern margin of Tibetan Plateau,is a Mesozoic marine petroliferous basin covering an area of 30 000 km2.The basin has been received little hydrocarbon interest for its severe climate and life conditions,although it situates in the east of Tethyan realm,which is concentrated about 70% of the total world petroleum resources.Measured section and geochemical ana-lysis are combined to better understand the hydrocarbon potential.Two major source rock units have been identified: the Upper Jurassic Menkadun Formation and the Lower Cretaceous Gangba Group.Their potential source rock successions,mainly composed of dark shales during Oxfordian-Tithonian and Aptian,respectively,were deposited in outer shelf.TOC content ranges from 0.67 to 1.62 weight percent with an average value of about 1.03 weight percent for the Menkadun Formation and 0.7 to 1.08 weight percent with an average value of about 0.86 weight percent for the Gangba Group.All shale samples are composed of a mixed typeⅡ1(oil prone) kerogen.The vitrinite reflectance data and biomarker suggest that the Gangba Group is at late mature with respect to petroleum generation and the Menkadun Formation is overmature with respect to liquid hydrocarbon generation.These data indicate the shales of the units are good potential source rocks.Therefore,the good source rocks supply abundant matters for the formation of oil and gas in this area.

     

    • FullText(HTML)
  • loading
    • References(36)
  • [1]
    王成善,张哨楠.青藏高原含油气盆地分析及油气资源预测[J].地球科学:中国地质大学学报,1996,21(2):120-129.
    [2]
    罗小平,朱剑如,祁开令.西藏岗巴-定日盆地找油前景[J].地球科学:中国地质大学学报,1996,21(2):158-162.
    [3]
    费琪,邓忠凡.西藏特提斯构造域海相油气前景[J].地球科学:中国地质大学学报,1996,21(2):113-119.
    [4]
    GRADSTEIN F M,GIBLING M R,SARTI M,et al.Mesozoic Tethyan strata of Thakkhola,Nepal:evidence for the drift and breakup of the Gondwana[J].Palaeogeography,Palaeoclimatology,Palaeoecology,1991,88(3-4):193-218.
    [5]
    GAETANI M,GARZANTI E.Multicyclic history of the northern India continental margin(northwestern Himalaya)[J].AAPG Bulletin,1991,75(9):1427-1446.
    [6]
    曾华盛,王津义.西藏岗巴盆地烃源岩评价[J].天然气工业,2003,23(6):16-21.
    [7]
    ROWLEY D B.Age of initiation of collision between India and Asia:A review of stratigraphic data[J].Earth and Planetary Science Letters,1996,145(1):1-13.
    [8]
    河北省地质调查院.中华人民共和国区域地质调查报告(1:25万日新幅、札达县幅、姜叶马幅)[R].石家庄:河北省地质调查院,2005.
    [9]
    LIU GUANGHUA,EINSELE G.Sedimentary history of the Tethyan basin in the Tibetan Himalayas[J].Geologische Rundschau,1994,83,32-61.
    [10]
    GARZANTI E.Stratigraphy and sedimentary history of the Nepal Tethys Himalaya passive margin[J].Journal of Asian Earth Sciences,1999,17(5-6):805-827.
    [11]
    西藏地质矿产局区域地质矿产调查大队.中华人民共和国区域地质调查报告(1:100万噶大克幅区域地质报告)[R].北京:地质出版社,1987.
    [12]
    郭铁鹰,梁定益,张宜智,等.西藏阿里地质[M].武汉;中国地质大学出版社,1991:66-85.
    [13]
    西藏地质矿产局.西藏自治区区域地质志[M].北京:地质出版社,1993:160-224.
    [14]
    西藏地质矿产局.西藏自治区岩石地层[M].武汉:中国地质大学出版社,1997:197-202.
    [15]
    万晓樵,赵文金,李国彪.对西藏岗巴上白垩统的新认识[J].现代地质,2000,14(3):281-285.
    [16]
    阴家润,万晓樵,金朝雯.东特提斯首条三叠-侏罗系界线剖面[C]//第三届全国地层会议论文集.北京:地质出版社,2000:179-185.
    [17]
    徐钰林,万晓樵,苟宗海,等.西藏侏罗纪,白垩纪,第三纪地层[M].武汉:中国地质大学出版社,1990.
    [18]
    李祥辉,王成善,万晓樵,等.西藏江孜县床得剖面侏罗-白垩纪的地层层序及地层划分[J].地层学杂志,1999,23(4):303-309.
    [19]
    LI XIANGHUI,WANG CHENGSHAN,HU XIUMIAN.Stratigraphy of deep-water Cretaceous deposits in Gyangze,southern Tibet,China[J].Cretaceous Research,2005,26(1):33-41.
    [20]
    GRADSTEIN F M,ULRICH V R.Stratigraphic evolution of Mesozoic continental margin and oceanic sequences:Northwest Australia and northern Himalayas[J].Marine Geology,1991,102(1-4):131-173.
    [21]
    JADOUL F,FABRIZIO B,GARZANTI E.The Tethys Himalayan passive margin from Late Triassic to Early Cretaceous(South Tibet)[J].Journal of Asian Earth Sciences,1998,16(2-3):173-194.
    [22]
    HU XIUMIAN,LUBA J,WANG CHENGSHAN.Upper Jurassic-Lower Cretaceous stratigraphy in south-eastern Tibet:a comparison with the western Himalayas[J].Cretaceous Research,2008,29(2):301-305.
    [23]
    苟宗海.略论西藏斯匹提页岩的地层分布[J].成都地质学院院报,1989,16(1):16-26.
    [24]
    WILLEMS H,ZHANG BINGGAO.Cretaceous and Lower Tertiary sediments of the Tibetan Tethys Himalaya in the area of Gamba(South Tibet,PR China)[D].Fachbereich Geowissenschaften,Universitat Bremen,1993:3-27.
    [25]
    秦建中,刘宝泉,国建英,等.关于碳酸盐烃源岩的评价标准[J].石油实验地质,2004,26(3):281-286.
    [26]
    邬立言,顾信章,盛志伟,等.生油岩热解快速定量评价[M].北京:科学出版社,1986:30-31.
    [27]
    庞雄奇,方祖康,陈章明.地史过程中的岩石有机质含量变化及其计算[J].石油学报,1988,9(1):17-24.
    [28]
    郝石生,高岗,王飞宇,等.高-过成熟海相烃源岩[M].北京:石油工业出版社,1996:98-109.
    [29]
    程克明,王兆云.高成熟和过成熟海相碳酸盐岩生烃条件评价方法研究[J].中国科学(D辑),1996,26(6):537-543.
    [30]
    秦建中,郑伦举,腾格尔.海相高演化烃源岩总有机碳恢复系数研究[J].地球科学:中国地质大学学报,2007,32(6):853-860.
    [31]
    岳来群,李永铁,史晓颖.西藏古错-岗巴盆地下白垩统黑色页岩地质特征及其油气资源意义[J].古地理学报,2006,8(3):307-316.
    [32]
    赵政璋,李永铁,叶和飞,等.青藏高原海相烃源层的油气生成[M].北京:科学出版社,2000.
    [33]
    王立成,王成善,李亚林,等.西藏措勤盆地色林错凹陷郎山组分子地球化学特征[J].沉积学报,2009,27(6):1199-1207.
    [34]
    秦建中,付小东,腾格尔.川东北宣汉-达县地区三叠-志留系海相优质烃源层评价[J].石油实验地质,2008,30(4):367-374.
    [35]
    TISSOT B P,WELTE D H.Petroleum formation and occurrence[M].Berlin:Springer-Verlag,1984:123-185.
    [36]
    JENKYNS H C.Cretaceous anoxic events:From continents to oceans[J].Journal of the Geological Society London,1980,137(2):171-188.
    • 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 (2049) PDF downloads(1028) 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