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Volume 24 Issue 5
Oct 2013
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Journal of Earth Science  > 2013  >  24(5): 815-829.
Libo Wang, Yeqian Zhang, Junjie Cai, Guangzhi Han. Characteristics of the Upper Jurassic Marine Source Rocks and Prediction of Favorable Source Rock Kitchens in the Qiangtang Basin, Tibet. Journal of Earth Science, 2013, 24(5): 815-829. doi: 10.1007/s12583-013-0375-5
Citation: Libo Wang, Yeqian Zhang, Junjie Cai, Guangzhi Han. Characteristics of the Upper Jurassic Marine Source Rocks and Prediction of Favorable Source Rock Kitchens in the Qiangtang Basin, Tibet. Journal of Earth Science, 2013, 24(5): 815-829. doi: 10.1007/s12583-013-0375-5
shu

Characteristics of the Upper Jurassic Marine Source Rocks and Prediction of Favorable Source Rock Kitchens in the Qiangtang Basin, Tibet

doi: 10.1007/s12583-013-0375-5
  • 1.

    Faculty of Earth Resources, China University of Geosciences, Wuhan, 430074, China

  • 2.

    Northeast Petroleum University, Daqing, 163318, China

  • 3.

    School of Energy Resources, China University of Geosciences, Beijing, 100083, China

  • 4.

    Key Laboratory for Marine Reservoir Evolution and Hydrocarbon Abundance Mechanism, Ministry of Education, China University of Geosciences, Beijing, 100083, China

  • 5.

    Baker Hughes, Drilling System, Rocky Mountain Area, Denver, CO, 80202, USA

Funds:

the National Natural Science Foundation of China 41372139

the National Natural Science Foundation of China 41072098

the National Natural Science Foundation of China 41002027

the National Major Projects of China 2011ZX05018-001-002

the National Major Projects of China 2011ZX05009-002-205

More Information
  • Corresponding author: Libo Wang, libowang2008@126.com
  • Received Date: 18 Oct 2012
  • Accepted Date: 25 Dec 2012
  • Publish Date: 01 Oct 2013
    Abstract
  • This study evaluated the hydrocarbon-bearing potential of Upper Jurassic marine source rocks in the Qiangtang (羌塘) Basin through a comprehensive organic geochemical analysis of the samples from a large number of outcrops in different structural units to predict the location of favorable hydrocarbon kitchens, based on the evaluation standards of Mesozoic marine source rocks in the Qiangtang Basin. Rocks' depositional environment, thickness and organic geochemistry feature were analyzed in this study. The principal controlling factors of the occurrences of favorable source rocks were analyzed. Upper Jurassic Suowa (索瓦) Formation source rocks are mainly platform limestone in the Dongcuo (洞错)-Hulu (葫芦) Lake deep sag and Tupocuo (吐坡错)-Baitan (白滩) Lake deep sag. Lithologically, the Suowa Fromation is made up of a suite of marls in intra-platform sags, micrites and black shales, which were all deposited in the closed, deep and static water depositional environment. Marl could form hydrocarbon-rich source rocks and its organic matter type is mainly Ⅱ type in mature to highly-mature stage, the limestone forms a medium-level source rock. In addition, the favorable source kitchen of limestone is larger than that of mudstone. This study provides an important reference for the evaluation of Jurassic marine source rocks and for prediction of petroleum resources in the Qiangtang Basin.

     

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