Titlebook: Mechanics Problems in Geodynamics Part II; Part II Ren Wang,Keiiti Aki Book 1996 Birkhäuser Verlag 1996 Deformation.Geodynamik.Geophysik.Se

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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

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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. Th

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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 (globall

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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