Abstract
In this paper, earthquake process is described as the process of local destabilization of system in mathematical and physical view and the critical conditions of local instability are given by variational principle. The unknown of basic properties, evolution characters and disturbance characters of crustal medium in deep and the non-completeness of human knowledge make great hardships in directly determining the stiffness and evolution of lithospheric medium. So an inversion strategy is proposed based on the distribution of a dense number of GPS sites and strain gauges.
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