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- W3151789535 abstract "Bohai 海湾盆在北方中国 Craton 是中生代沉淀和新生代裂缝盆。自从 Permo 含碳的烃来源岩石的免职，盆经历了许多构造事件。来源岩石经历了不一致高举，扭动，深埋葬，并且 magmatism 和导致那一打断或在烃来源岩石的进化期间逐步。我们调查了埋葬的 Permo 含碳的烃来源岩石历史，加热，并且烃产生，不是仅仅根据构造骚乱并且深深地埋葬了而且与容易的 % Ro 的数字模拟的磷灰石分裂磁道分析，液体包括大小，和应用程序上的新研究。来源岩石的加热温度继续从 Indosinian 升起到喜玛拉雅的舞台并且到达了最大值在晚喜玛拉雅。这在器官的成熟和烃产生的多重阶段期间导致了逐步的增加。学习描出构造阶段，烃产生的紧张和烃代的空间、时间的分发。烃产生发生在 Indosinian 期间， Yanshanian，并且特别地迟了喜玛拉雅。烃产生在晚喜玛拉雅的阶段期间是为在中国的 Bohai 海湾盆的 Permo 含碳的来源岩石的最重要的。" @default.
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- W3151789535 date "2010-01-01" @default.
- W3151789535 modified "2023-09-23" @default.
- W3151789535 title "Hydrocarbon Generation Evolution of Permo-Carboniferous Rocks of the Bohai Bay Basin in China" @default.
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