Asymmetric dynamics at subduction zones derived from plate kinematic constraints
Abstract
The lithospheric sinking along subduction zones is part of the mantle convection. Therefore, computing the volume of lithosphere recycled within the mantle by subducting slabs quantifies the equivalent amount of mantle that should be displaced, for the mass conservation criterion. The rate of subduction is constrained by the convergence rate between upper and lower plates and the motion of the subduction hinge H that may either converge or...
Paper Details
Title
Asymmetric dynamics at subduction zones derived from plate kinematic constraints
Published Date
Feb 1, 2020
Journal
Volume
78
Pages
110 - 125
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