烃源岩有机质热演化过程中碳氢含量的变化

1993年 14卷 第No.3期
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H/C CONTENT VARIATION OF ORGANIC MATTER IN SOURCE ROCKS DURING THERMAL EVOLUTION
王新洲
Wang Xinzhou
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()求出烃源岩降解残碳率和氢碳原子比的经验方程。
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.
干酪根; 有机质热演化; 降解残碳率; H/C—Ro关系;
10.11743/ogg19930307