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- W3140714912 abstract "Neotectonic 运动指自从新生代，发生了的构造运动，它是最近的运动。它在西方中国在盆上有最重要的影响，特别在在西方的低岬盆的烃累积上。我们在 Kuqa 低岬盆决定了 neotectonic 运动的时间，它从晚第三纪开始了，并且分析了运动的模式，它是在垂直方向和强烈侧面的压缩的连续、快的沉淀。结构式样是指责被削弱，合拢从北方逐渐地被加强到南方。我们与盆模拟技术在 Kuqa 低岬盆在烃累积过程和模型上学习了 neotectonic 运动的控制。Kuqa 低岬盆的最大的沉淀率在 neotectonic 运动期间到达了 1,200 m/Ma，导致 5 妈和烃的大数量正在被产生并且驱逐的在内的来源岩石的快速的成熟。厚 neotectonic 阶层能分别地为 5% 全部的储备和 27% 与证明气体和油储备财务形成高质量的水库。86% 结构的陷井在 neotectonic 运动时期被形成。在 neotectonic 运动期间形成的差错用作重要迁居小径，他们在烃水库是分布式的区域存在。反常地高的压力由强烈侧面的压缩，厚 neotectonic 阶层免职和快速的烃产生引起了为烃移植提供驱动力。累积元素在一个短时期上匹配对方很好，导致以后在 Kuqa 低岬盆形成的许多大煤气的域。" @default.
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- W3140714912 date "2010-01-01" @default.
- W3140714912 modified "2023-09-24" @default.
- W3140714912 title "Control of neotectonic movement on hydrocarbon accumulation in the Kuqa Foreland Basin, west China" @default.
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