caa a22 4500 445302763 CHVBK 20180317142603.0 cr unu---uuuuu 170323e20101201xx s 000 0 eng 10.1134/S0001433810080062 doi (NATIONALLICENCE)springer-10.1134/S0001433810080062 Deep structure of the Moscow Aulacogene in the western part of Moscow [Elektronische Daten] [E. Rogozhin, A. Gorbatikov, N. Larin, M. Stepanova] Geological and geomorphological studies of the Moscow Aulacogene in the western part of Moscow suburbs have been conducted. This deep structure has been studied by microseismic sounding. The resulting section presents the faults which frame the Teplostanskii Graben in the south (Ramenskii or Butovskii, expressed on the surface as a ledge in the relief) and in the north (Pavlovo-Posadskii, being traced on the surface as a series of lineaments and the valley of Setun' River). The position of the surface Archean-Lower Proterozoic crystalline basement within the limits of the graben and within the limits of buried elevated blocks (Krasnogorskii and Tumsk-Shaturskii) frame it in the north and south, respectively. Additionally, another fault has been identified in the central part of the graben: the Solntsevskii fault, which has a north-western course and which separates the deflection of the basement in two blocks that are sunken in a slightly different degree. The low-velocity horizons of the Riphean-Vendian complex which make up the graben at depths of 2 to 4.5 km have been found. Down to depths of 15 km, as a component of the upper crust, the graben is underlain by a high-velocity material which also forms the upper part of the section of the crystalline basement in the neighboring elevated block. A low-velocity block of the lithosphere is located in the larger (northern) part of the graben deeper (down to 40 km) beneath the zones of Pavlovo-Posadskii and Solntsevskii faults; in the southern part there is a high-velocity block. In the fault zones framing the graben in the north and south, the surface layer and soil displays a flow of juvenile hydrogen and helium which exceeds several tenfold the background values. According to the collected data, the Teplostanskii Graben has roots traceable through the entire crust and penetrating into the upper mantle. Pleiades Publishing, Ltd., 2010 Moscow Aulacogene nationallicence Teplostanskii Graben nationallicence deep structure nationallicence microseismic sounding nationallicence juvenile hydrogen nationallicence Rogozhin E. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia aut Gorbatikov A. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia aut Larin N. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia aut Stepanova M. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia aut Izvestiya, Atmospheric and Oceanic Physics SP MAIK Nauka/Interperiodica 46/8(2010-12-01), 973-981 0001-4338 46:8<973 2010 46 11485 https://doi.org/10.1134/S0001433810080062 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1134/S0001433810080062 text/html Onlinezugriff via DOI NATIONALLICENCE 700 1- Rogozhin E. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia aut NATIONALLICENCE 700 1- Gorbatikov A. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia aut NATIONALLICENCE 700 1- Larin N. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia aut NATIONALLICENCE 700 1- Stepanova M. Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia aut NATIONALLICENCE 773 0- Izvestiya, Atmospheric and Oceanic Physics SP MAIK Nauka/Interperiodica 46/8(2010-12-01), 973-981 0001-4338 46:8<973 2010 46 11485 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer