2007Acta Scientiarum Naturalium Universitatis SunyatseniRequires access

Mechanism of Silurian Hydrocarbon Pool Formation in the Tarim Basin

Liu, Luofu, Chen, Yuanzhuang, Lixin, Pang, Xiongqi, Xie, Qilai, Huo, Hong, Zhao, Suping, Li, Chao, Shuangwen, Guo -, Yongqiang

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Abstract

有在 Tarim 盆的志留纪烃水池的三个形成阶段。在 Tazhong (中央 Tarim ) 和 Tabei (北 Tarim ) 的广泛地分布式的柏油的沙岩区域是形成在的烃水池的破坏的结果第一阶段,并且在 Awati 附近的柏油的沙岩下垂在秒阶段被形成。烃迁居特征在志留纪 paleo 水池由干燥沥青能代表的剩余反映了烃的迁居特征,当在志留纪水库的现在的活动的油与有关时以后阶段(第三阶段) 烃累积。

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What this paper is about

有在 Tarim 盆的志留纪烃水池的三个形成阶段。在 Tazhong (中央 Tarim ) 和 Tabei (北 Tarim ) 的广泛地分布式的柏油的沙岩区域是形成在的烃水池的破坏的结果第一阶段,并且在 Awati 附近的柏油的沙岩下垂在秒阶段被形成。烃迁居特征在志留纪 paleo 水池由干燥沥青能代表的剩余反映了烃的迁居特征,当在志留纪水库的现在的活动的油与有关时以后阶段(第三阶段) 烃累积。

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Available abstract

有在 Tarim 盆的志留纪烃水池的三个形成阶段。在 Tazhong (中央 Tarim ) 和 Tabei (北 Tarim ) 的广泛地分布式的柏油的沙岩区域是形成在的烃水池的破坏的结果第一阶段,并且在 Awati 附近的柏油的沙岩下垂在秒阶段被形成。烃迁居特征在志留纪 paleo 水池由干燥沥青能代表的剩余反映了烃的迁居特征,当在志留纪水库的现在的活动的油与有关时以后阶段(第三阶段) 烃累积。

Key concepts: Tarim basin, Geology, Mechanism (biology), Ordovician, Paleontology, Epistemology, Philosophy

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