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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. 其有機地球化學環境蓡數分析表明，這兩套沉積其形成於缺氧還原的微鹹水鹹水的半深湖深湖環境，是盆地主要的烴源巖系。