METHOD FOR REGIONAL SEISMIC INVESTIGATIONS

摘要

use: u0440u0435u0433u0438u043eu043du0430u043bu044cu043du0430u00a0 seismic prospecting study of geological u0441u0442u0440u043eu0435u043du0438u00a0 u0441u043bu043eu0436u043du043eu043fu043eu0441u0442u0440u043eu0435u043du043du044bu0445 environments.the essence of the u0438u0437u043eu0431u0440u0435u0442u0435u043du0438u00a0: regional profiles are in the form of pairs of u043au0432u0430u0437u0438u043fu0430u0440u0430u043bu043bu0435u043bu044cu043du044bu0445 piecewise continuous profiles and lateral profiles are in the form of u043fu0435u0440u0435u0441u0435u043au0430u044eu0449u0438u0445u0441u00a0 friend other piecewise continuous profiles, are taking the lateral profiles for u043fu0440u043eu0441u0442u0438u0440u0430u043du0438u044e produced by these tectonic elements are around these elements u0437u0430u043cu043au043du0443 the landfillthe position of each subsequent pair of profiles u0443u0442u043eu0447u043du00a0u044eu0442 after u043fu043eu043bu0443u0447u0435u043du0438u00a0 data in the previous couple of profiles, and u0440u0430u0441u0441u0442u043eu00a0u043du0438u0435 between regional u043fu0440u043eu0444u0438u043bu00a0u043cu0438 oprah u0434u0435u043bu00a0u044eu0442 size of tectonic elements. 1 il.