石油与天然气地质 ›› 1993, Vol. 14 ›› Issue (3): 223-228.doi: 10.11743/ogg19930307

• 论文 • 上一篇    下一篇

烃源岩有机质热演化过程中碳氢含量的变化

王新洲   

  1. 胜利石油管理局地质科学研究院 山东 东营257015
  • 收稿日期:1990-05-21 修回日期:1990-07-28 出版日期:1993-09-25 发布日期:2012-01-16

H/C CONTENT VARIATION OF ORGANIC MATTER IN SOURCE ROCKS DURING THERMAL EVOLUTION

Wang Xinzhou   

  1. Geological Research Institute, Shengli Petroleum Administration, Dongying, Shandong
  • Received:1990-05-21 Revised:1990-07-28 Online:1993-09-25 Published:2012-01-16

PDF (PC)

800

被引次数

4

摘要：

本文通过对大量地化数据(包括模拟试验数据)的回归分析,给出了根据干酪根类型和成熟度(Ro)求出烃源岩降解残碳率和氢碳原子比的经验方程。

关键词: 干酪根, 有机质热演化, 降解残碳率, H/C—Ro关系

Abstract:

According to geochemical data (including the data of simulated test of thermal degradation),the correlations between vitrinite reflectance and organic matter/residual carbon,H/C in kerogen were discussed and 13 correspoundent regression equations were given in this paper.