Volume 26 Issue 6
Dec.  2020
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Article Contents
HU Jinjie, TANG Youjun, HE Daxiang, et al., 2020. Comparison and exploration of hydrocarbon expulsion patterns of different types of source rocks. Journal of Geomechanics, 26 (6): 941-951. DOI: 10.12090/j.issn.1006-6616.2020.26.06.075
Citation: HU Jinjie, TANG Youjun, HE Daxiang, et al., 2020. Comparison and exploration of hydrocarbon expulsion patterns of different types of source rocks. Journal of Geomechanics, 26 (6): 941-951. DOI: 10.12090/j.issn.1006-6616.2020.26.06.075

Comparison and exploration of hydrocarbon expulsion patterns of different types of source rocks

doi: 10.12090/j.issn.1006-6616.2020.26.06.075
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  • Received: 2020-04-22
  • Revised: 2020-06-05
  • Published: 2020-12-01
  • Hydrocarbon expulsion from source rocks is a very important part in the accurate prediction of oil and gas resources in petroliferous basins. In order to obtain the hydrocarbon expulsion efficiency and mechanism, the source rocks of different organic matter types were selected for the gold tube simulation experiments, product change characteristics and hydrocarbon expulsion efficiency of different types of source rocks in different evolution stages are summarized. The results show that, the type has a great influence on the proportion of light and heavy hydrocarbons in total oil and residual oil, but has little on that in discharged oil; the discharged oil is dominated by heavy hydrocarbons in the immature-mature stage and light hydrocarbons in the high-mature-overmature stage. The type has obvious influence on the amount of oil generation and discharge. The better the type of source rock is, the higher the amount of oil generation and discharge is. The oil generation and discharge amount of typeⅠsource rocks is the highest and that of typeⅢsource rocks is the lowest. The better the type of source rock is, the higher the oil discharge efficiency is. The low oil discharge efficiency of typeⅢsource rocks is related to the high generation of gaseous hydrocarbon and the high content of vitrinite in macerals.

     

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