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Late Cenozoic tectonic deformation in the Tianshan Mountain and its foreland basins

机译:天山及其前陆盆地晚新生代构造变形

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摘要

The magnificent Tianshan Mountain has owned its respects and high praise since the beginning of ancient Chinese civilization. When the history wheeled into the 1990s, a large group of earth scientists once again focused their sights on the Tianshan Mountain, the most spectacular Cenozoic rejuvenated intra-plate mountain building. Why does such strong tectonic deformation occur in the continental interior several thousand kilometers away from plate boundaries? What are the pattern and magnitude of thetectonic deformation? What factors dominate tectonic deformation in the continental interior? How do the dynamic processes at the depth dictate tectonic deformation near the surface? The Tianshan Mountain provides a natural laboratory to answer these important scientific questions.
机译:自中国古代文明开始以来,宏伟的天山就已享有崇高的敬意。当历史进入1990年代时,一大群地球科学家再次将目光投向了天山,这是最壮观的新生代复兴的板内山建筑。为什么在距板块边界几千公里的大陆内部会发生如此强烈的构造变形?构造变形的模式和大小是什么?哪些因素主导了大陆内部的构造变形?深度处的动力学过程如何指示地表附近的构造变形?天山提供了一个天然的实验室来回答这些重要的科学问题。

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