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    Volume 36 Issue 1
    Jan.  2011
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    PING Hong-wei, CHEN Hong-han, 2011. Main Controlling Factors on Oil Inclusion Homogenization Temperatures and Their Geological Significance. Earth Science, 36(1): 131-138. doi: 10.3799/dqkx.2011.014
    Citation: PING Hong-wei, CHEN Hong-han, 2011. Main Controlling Factors on Oil Inclusion Homogenization Temperatures and Their Geological Significance. Earth Science, 36(1): 131-138. doi: 10.3799/dqkx.2011.014

    Main Controlling Factors on Oil Inclusion Homogenization Temperatures and Their Geological Significance

    doi: 10.3799/dqkx.2011.014
    • Received Date: 2010-06-09
    • Publish Date: 2011-01-01
    • Petroleum inclusions trapped in diagenetic minerals have been extensively applied to studies of constraint hydrocarbon migration and accumulation, but the effects on petroleum inclusion homogenization temperatures and their geological implications have not been completely understood. In this paper, a thermodynamic modeling method was employed, and two types of black oil and volatile oil were used to simulate their homogenization temperatures and to establish the homogenization temperature relationship between petroleum inclusions and their coeval aqueous inclusions under different P-T conditions. It is concluded that all the petroleum composition, trapped temperature and pressure have influence on the petroleum inclusion homogenization temperature. In contrast, if the trapped P-T and petroleum composition of single inclusion are known, the petroleum inclusion homogenization temperature and the difference between petroleum inclusions and their coeval aqueous inclusions can give geological meanings, which can play a great role on hydrocarbon charging episodes and paleofluid pressure modeling.

       

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