煤演化程度处于成熟—过成熟阶段。
The coal evolution is in stage of maturity to over-maturity.
沉积环境和构造运动对有机质丰度和热演化程度影响较大。
Sedimentary environment and tectonic movement have great influence on abundance and thermal evolution extent of organic matters.
包裹体类型和成分的不同，反映了油气的不同演化程度和不同运移期次。
Different types and composition of inclusions reflect different oil-gas evolution level and oil-gas migration in different phases.
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