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首页> 外文期刊>Geophysical Research Letters >Segmentation of the Main Himalayan Thrust Illuminated by Bayesian Inference of Interseismic Coupling
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Segmentation of the Main Himalayan Thrust Illuminated by Bayesian Inference of Interseismic Coupling

机译:贝叶斯耦合耦合衰退引起的主要喜马拉雅推力的分割

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摘要

We use a recent compilation of geodetic data of surface displacements in a fully Bayesian approach to derive a probabilistic estimate of interseismic coupling along the Main Himalayan Thrust (MHT). Our probabilistic estimate of interseismic coupling highlights four large, highly coupled patches separated by three potential barriers of low coupling. Locked patches overlap with estimated rupture areas of historical large earthquakes over the past centuries. The coincident spatial variability in coupling, seismicity, and prominent active topography suggests a structural segmentation of the MHT imposed by inherited tectonic structures from the India-Eurasia collision. This correlation implies that inherited tectonic structures may affect how stress builds up along the MHT, thereby influencing the location and size of large Himalayan earthquakes and the growth of the mountain range.
机译:我们使用最近汇编了表面位移的地理位置,以完全贝叶斯方法来得出沿着喜马拉雅推力(MHT)的主学耦合的概率估计。 我们对沉重耦合的概率估计突出了四个具有三个低耦合屏障的三个大型高耦合贴片。 过去几个世纪以来,锁定补丁重叠了历史大地震的估计破裂区域。 耦合,地震性和突出的主动形貌的重合空间可变性表明,由印度 - 欧亚碰撞的继承构造结构所施加的MHT结构分割。 这种相关性意味着继承的构造结构可能会影响压力沿着MHT的压力,从而影响大喜马拉雅大地震的位置和大小和山脉的生长。

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