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The parameters of organic geochemistry indicated that the two sets of source rocks were deposited in the bathybic and bathyal milieu with the subsaline-saline water. 其有机地球化学环境参数分析表明，这两套沉积其形成于缺氧还原的微咸水咸水的半深湖深湖环境，是盆地主要的烃源岩系。