Guo Dixiao, Feng yuanzheng. IS VITRINITE REFLECTANCE THE GENERAL CRITERION OF MATURATION?[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1990, 12(4): 421-425. doi: 10.11781/sysydz199004421
Citation: Guo Dixiao, Feng yuanzheng. IS VITRINITE REFLECTANCE THE GENERAL CRITERION OF MATURATION?[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1990, 12(4): 421-425. doi: 10.11781/sysydz199004421

IS VITRINITE REFLECTANCE THE GENERAL CRITERION OF MATURATION?

doi: 10.11781/sysydz199004421
  • Received Date: 1989-06-17
  • Publish Date: 1990-10-25
  • Through thermal simulation experiments on organics of different types, the authors found that there were much difference in vitrinite reflectance for different organics subjected to same thermal evolution. The difference for R°could reach as much as 0.24-0.60 with same thermal gradient. At low thermal stage (360℃), the values of R° for type I were lower than those for type Ⅲ;and at high thermal stage, with contrary results come about. This phenomena tallies with the observations from field sections, suggesting that vitrinite reflectance is influenced by the type of parent material. In view of above-mentioned facts,vitrinite reflectance as a general "criterion" for maturity can be applicable only for the same kind of organics, but it is difficult to use it in comparisions of different types of organics, therefore it can not be taken as a general "criterion", and correction need to be made.

     

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    赵师庆等,1987,不同煤相中煤和镜质组特征的初步研究,中国科学院地球化学所1987年研究年报,科学出版社.
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    J.W.史密斯,1988.预测石油远景的参数选择,石油实验地质,第10卷第4期.
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