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Abstract

Paleothermic conditions are a most responsible factor for the generation, accumulation and preservation of hydrocarbons. These conditions determine a thermal maturity of organic matter and its hearing deposits.

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/content/papers/10.3997/2214-4609.201408537
1998-06-08
2024-04-25
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408537
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