The evolution history of the palaeogeotemperature field of a basin is one of the decisive factors which control the process in which organic matter turns to hydrocarbon and the hydrocarbon preserves as well as migrales.
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释义
盆地古地温场的演化史是盆地有机质向烃类转化以及烃类保存或变迁的决定性控制因素之一。
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