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METHOD FOR PREDICTING SOURCE ROCK BY PALEOENVIRONMENT RESTORATION

机译:利用古环境恢复预测烃源岩的方法

摘要

A method for predicting a source rock by paleoenvironment restoration includes: (1) measuring a content of each mineral; (2) judging whether a sedimentary environment is a marine facies or a non-marine facies by utilizing element combination forms of Sr/Ba, B/Ga, Th/U, Fe/Mn and Sr/Ca; (3) judging a specific numerical value of a paleosalinity through a boron element and comparing the same with a current normal seawater value to deduce whether the current sedimentary environment is a saline water or non-saline water sedimentary environment; (4) judging an oxidation or reduction environment during sedimentation through element combination forms of (Cu+Mo)/Zn and V/(V+Ni); and (5) comprehensively analyzing the sedimentary environment, restoring a relationship between a palaeosedimentary environment and a source-reservoir configuration.
机译:一种通过古环境恢复预测烃源岩的方法包括:(1)测量每种矿物的含量;(2) 利用Sr/Ba、B/Ga、Th/U、Fe/Mn和Sr/Ca元素组合形式判断沉积环境是海相还是非海相;(3) 通过硼元素判断古盐度的特定数值,并将其与当前正常海水值进行比较,以推断当前沉积环境是盐水沉积环境还是非盐水沉积环境;(4) 通过(Cu+Mo)/Zn和V/(V+Ni)的元素组合形式判断沉淀过程中的氧化或还原环境;(5)综合分析沉积环境,恢复古沉积环境与生储结构的关系。

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