A method of predicting earthquake parameters

摘要

method u043fu0440u043eu0433u043du043eu0437u0438u0440u043eu0432u0430u043du0438u00a0 parameters u0437u0435u043cu043bu0435u0442u0440u00a0u0441u0435u043du0438u00a0 comprising obtaining images on two mutually u043eu0440u0442u043eu0433u043eu043du0430u043bu044cu043du044bu043c on u043fu043eu043bu00a0u0440u0438u0437u0430u0446u0438u0438 channels set, u0444u043eu0440u043cu0438u0440u043eu0432u0430 we synthesised the matrix u0438u0437u043eu0431u0440u0430u0436u0435u043du0438u00a0 u043fu043eu043fu0438u043au0441u0435u043bu044cu043du044bu0445 amplitudes of signals u043fu043eu043bu00a0u0440u0438u0437u0430u0446u0438u043eu043du043du044bu0445 channels, processing of the matrix u0441u0438u043du0442u0435u0437u0438u0440u043eu0432u0430u043du043du043eu0433u043e u0438u0437u043eu0431u0440u0430u0436u0435u043du0438u00a0, distinguishes u0441u00a0 orderwhat u0432u044bu0447u0438u0441u043bu00a0u044eu0442 expectation signals of images u043fu043eu043bu00a0u0440u0438u0437u0430u0446u0438u043eu043du043du044bu0445 channels, u0441u0438u043du0442u0435u0437u0438u0440u043eu0432u0430u043du043du0443u044e matrix form of u043fu043eu043fu0438u043au0441u0435u043bu044cu043du044bu0445 relations and u0441u0438u0433u043d ala with great mathematical expectation of less consistently from the beginning up u0438u0437u043eu0431u0440u0430u0436u0435u043du0438u00a0 synthetic matrix for fragments of four related u043fu0438u043au0441u0435 la,u0434u0435u043bu00a0u0442 every square inch to two adjacent triangle and heron's formula u0432u044bu0447u0438u0441u043bu00a0u044eu0442 size, u043du0430u0445u043eu0434u00a0u0442 elevation area (sp) surface u0438u0437u043eu0431u0440u0430u0436u0435u043du0438u00a0 as the amount of triangles all mosaic fragments on a series of consecutive in time image tracking function u0448u0435u0440u043eu0445u043eu0432u0430u0442u043e u0438u0437u043cu0435u043du0435u043du0438u00a0 dynamics. ste terrainon the basis u0432u044bu0447u0438u0441u043bu00a0u044eu0442 u043fu043eu0441u0442u043eu00a0u043du043du0443u044e exhibitors are the observed process are expected u0432u0440u0435u043cu00a0 impact ty4,6T and its magnitude (m) of the u0441u043eu043eu0442u043du043eu0448u0435u043du0438u00a0 lgty [cym] = 0,54u043c - 3,37 where t2 - t1 = t is the time interval between successive exposures u0434u0432u0443u043cu00a0, h; d1, d2 is computed as the roughness of terrain in the times t2, t1; 2001 - limit of roughness of surface terrainwhere is the "u0432u0441u043fu0430u0440u0438u0432u0430u043du0438u0435" hearth; S0 area u0438u0437u043eu0431u0440u0430u0436u0435u043du0438u00a0 synthetic matrix of pixels.