1.method u0432u044bu00a0u0432u043bu0435u043du0438u00a0 zone u043du0430u0445u043eu0436u0434u0435u043du0438u00a0 "u00a0u0437u044bu043au0430" u0434u0438u0430u043fu0438u0440u0430 u043cu0430u043du0442u0438u0439u043du043eu0433u043e substances u0437u0430u043au043bu044eu0447u0430u044eu0449u0438u0439u0441u00a0 in areas u0440u0438u0444u0442u043eu0433u0435u043du0435u0437u0430, u043fu043eu0434u043fu0435u0440u0442u044bu0445 u0434u0438u0430u043fu0438u0440u0430u043cu0438 anomalous mantle,u043fu0440u043eu0432u043eu0434u00a0u0442 geological u043du0430u0431u043bu044eu0434u0435u043du0438u00a0 and on the availability of u0432u043eu0437u0434u0435u0439u0441u0442u0432u0438u00a0 jets u0441u0438u043bu0430u043du043eu0432 on mountain rocks and / or the existence of isolated ranges of up to 200 u043fu0440u043eu0442u00a0u0436u0435u043du043du043eu0441u0442u044c km to 20 km in width and / or the footsteps of u0441u0438u043bu0430u043du043eu0432 and / or on the presence of slag cones u043eu043fu0440u0435u0434u0435u043bu00a0u044eu0442 place u043du0430u0445u043eu0436u0434u0435u043du0438u00a0 "u00a0u0437u044bu043au0430" substances of the mantle in the earth's crust, u043eu0442u043bu0438u0447u0430u044eu0449u0438 u0439u0441u00a0 orderwhat u0434u043bu00a0 u043eu043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 silicides at low depths as the physical parameters of u043eu043fu0440u0435u0434u0435u043bu0435u043du0438u00a0 places u043du0430u0445u043eu0436u0434u0435u043du0438u00a0 "u00a0u0437u044bu043au0430" substances in the earth's crust to the mantle u043eu043fu0440u0435u0434u0435u043bu00a0u044eu0442 line 3He / 4u043du0435 of gases selected sources u043fu043eu0440u00a0u0434u043au0430 10 - 5, and further establish the existence of a high electrical conductivity at the level of u043fu043eu043bu0443u043fu0440u043eu0432u043eu0434 ballet class, u043bu043eu043au0430u043bu044cu043du043eu0441u0442u044c and intensity of magnetic anomalyanomalies u043fu043eu043bu00a0 force u0442u00a0u0436u0435u0441u0442u0438 and depth u0437u0430u043bu0435u0433u0430u043du0438u00a0 silicides u043eu043fu0440u0435u0434u0435u043bu00a0u044eu0442 u043cu0430u0433u043du0438u0442u043eu0442u0435u043bu043bu0443u0440u0438u0447u0435u0441u043au0438u043c sensing and / or seismic methods reflected and u043fu0440u0435u043bu043eu043cu043bu0435u043du043du044bu0445 the waves.;2. method for u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0 1, so that an additional set of u0430u0440u0435u0430u043bu044cu043du043eu0433u043e u0432u0443u043bu043au0430u043du0438u0437u043cu0430.;3. method for u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0 1, so that an additional set of u043fu0440u0438u043fu043eu0432u0435u0440u0445u043du043eu0441u0442u043du044bu0445 explosions u0441u0438u043bu0430u043du043eu0432 as u043au0443u043cu0443u043bu00a0u0442u0438u0432u043du044bu0445 sinkholes on the up u0431u0430u0437u0430u043bu044cu0442u0430u0445.;4. method for u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0 1, so that an additional set of low u043eu0431u0432u043eu0434u043du0435u043du043du043eu0441u0442u0438 territories.;5. method for u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0 1, so that an additional set of low temperature gradients.;6. method for u043eu0442u043bu0438u0447u0430u044eu0449u0438u0439u0441u00a0 1, so that an additional set of u0430u0441u0435u0439u0441u043cu0438u0447u043du043eu0441u0442u0438 territories.
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