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- W2000570509 abstract "Abstract A fault zone is considered an open nonequilibrium dynamic system in which its constituent subsystems evolve by self-organization in a nonlinear synergetic process of successive changes of structural levels (stages). A new term fault dissipative structure is suggested for an ordered 3D space-time structure produced in a fault zone by self-organization of fracturess of different scales. The approach is used in physical modeling to simulate the evolution of a strike-slip fault zone in an elastic-viscoplastic lithosphere and to recognize space and time criteria diagnostic of fault dissipative structures through fractal and entropy analyses." @default.
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- W2000570509 date "2008-02-01" @default.
- W2000570509 modified "2023-10-17" @default.
- W2000570509 title "Dissipative structures in fault zones and their diagnostic criteria (from physical modeling data)" @default.
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- W2000570509 doi "https://doi.org/10.1016/j.rgg.2008.01.005" @default.
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