Abstract

The geological and geophysical study of the representative segment of the Alpine-Himalayan mobile belt—the Central zone of the Garhwal Himalaya—was conducted. The results of structural and geological studies in conjunction with the data on the deep structure obtained by geophysical methods, compared the speed of horizontal movements and the position of the hypocenters of seismic events, are presented. The successive decrease in the current rates of transverse compression is observed as we approach the maximum topographical heights of the geological and geophysical profile stretching across the Garhwal Himalaya. The large fault zones are shown, to which are related the foci of deep earthquakes.

中文翻译：

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Garhwal喜马拉雅山（印度）的深部构造和折块构造：综合地质和地球物理研究的结果

摘要

进行了高山-喜马拉雅移动带代表段（Garhwal喜马拉雅山的中部地区）的地质和地球物理研究。结合地球物理方法获得的深层结构数据，进行了结构和地质研究的结果，比较了水平运动的速度和地震事件震源的位置。随着我们接近横跨Garhwal喜马拉雅山的地质和地球物理剖面的最大地形高度，观察到了当前横向压缩率的连续下降。显示了大断层带，与深地震的震源有关。