有机质热演化程度普遍较高，应以天然气勘探为主。
Owing to high evolution of organic matte the main target in this region is gas survey.
镜质体反射率是用来反映有机质热演化史的主要指标。
The vitrinite reflectance is considered as an important index reflecting the thermo-evolution history of organic materials.
超压对有机质热演化的各个方面均未产生可识别的影响。
Overpressure had no detectable effect on All aspects of OM maturation.
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