Uppermost mantle structure and its relation with seismic activity in the central Tien Shan
【摘要】:正[1]Using arrival data from GHENGIS and Kyrgyz Network(KNET) stations,we determined the uppermost mantle structure of the central Tien Shan from Pn tomography.Pn velocities in the north-central Tien Shan are slower than normal for stable lithosphere.They are very slow in the south-central Tien Shan,where a hot mantle previously has been postulated.The Pn velocity variation
【相似文献】 | ||
|
|||||||||||||||||||||
|
|
|||||||||||||||||||||
|