Abstract Ingv


InSAR images allow to detect the coseismic deformation, delimiting the epicentral area where the larger displacement has been concentrated. By inspecting the InSAR fringe patterns is commonly recognized that, for dip-slip faults, the most deformed area is elliptical, or quadrilobated for strike-slip faults. This area coincides with the surface projection of the volume coseismically mobilized […]

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