ciliary-body 发表于 2025-3-27 00:20:30
Stress Field and Seismicity in the Indian Shield: Effects of the Collision between India and Eurasi The mean orientation of the maximum horizontal compression in the Indian subcontinent is subparallel to the direction of the ridge push at the plate boundary as well as to the direction of compression expected to arise from the net resistive forces at the Himalayan collision zone, indicating that t防水 发表于 2025-3-27 02:49:18
http://reply.papertrans.cn/63/6284/628395/628395_32.pngcalorie 发表于 2025-3-27 09:07:33
http://reply.papertrans.cn/63/6284/628395/628395_33.png暂时中止 发表于 2025-3-27 13:15:29
Mantle Flow with Existence of Plates and Generation of the Toroidal Field,toroidal field expresses the shearing of surface plates. One very important consideration in modeling flow in the earth’s mantle is the existence and motion of the lithospheric plates. The motion of plates represents a large-scale circulation with strong viscous coupling to the mantle underneath. ThLAVE 发表于 2025-3-27 16:44:32
http://reply.papertrans.cn/63/6284/628395/628395_35.png全神贯注于 发表于 2025-3-27 19:08:22
Dynamics of the Mid-ocean Ridge Plate Boundary: Recent Observations and Theory,ry is one of the most important problems in geodynamics. In this paper I present recent results of several aspects of mid-ocean ridge studies concerning the dynamics of oceanic lithosphere at these diverging plate boundaries. I show that the observed rift valley to no-rift valley transition (globallMEAN 发表于 2025-3-27 22:10:00
http://reply.papertrans.cn/63/6284/628395/628395_37.pngconscribe 发表于 2025-3-28 02:47:01
http://reply.papertrans.cn/63/6284/628395/628395_38.png慷慨不好 发表于 2025-3-28 07:27:18
http://reply.papertrans.cn/63/6284/628395/628395_39.png保留 发表于 2025-3-28 13:04:42
An Effective Approach to Determine the Dynamic Source Parameters,t assume that the kinematic source parameters, i.e., the slip and rupture time distributions on the fault plane, are known from the previous source inversion studies. Then, using the seismic source representation theorem we determine the dynamic stress field on a fault plane from known kinematic par