The crust and upper mantle structure beneath the Himalaya orogenic belt: The result from local earthquake data analysis
喜马拉雅造山带的地壳上地幔结构——近震反射观测结果

The broadband seismic observation through Himalaya was started in 2002 and ended in 2005.The stations are deployed closely along the profile and the reflection wave data of local earthquakes was collected.There is an important significance for studying velocity interfaces inside the crust and upper mantle.The data show that the most earthquakes in Qinghai-Tibet plateau happened in the upper crust.The ProP-arrivals and SmS-arrivals of the reflections from Moho in plateau are very clear with strong energy.The...