About thermodynamic evolution of Еarth crust and tectonic plates
Based on thermodynamic analysis of the geological structure, PT conditions on the earth's surface, and the powers that cause tectonic drift of continental and oceanic plates, presented physical and chemical regularity of evolution geospheres. These mainly related to the space powers of the Eart...
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Subbotin Institute of Geophysics of the NAS of Ukraine
2016
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fturanojs:oai:ojs.journals.uran.ua:article/91900 2023-05-15T18:23:12+02:00 About thermodynamic evolution of Еarth crust and tectonic plates Belevtsev, R.Ya. Blajko, V.I. Terechenko, S.I. 2016-12-01 application/pdf http://journals.uran.ua/geofizicheskiy/article/view/91900 rus rus Subbotin Institute of Geophysics of the NAS of Ukraine http://journals.uran.ua/geofizicheskiy/article/view/91900/87678 http://journals.uran.ua/geofizicheskiy/article/view/91900 Copyright (c) 2020 Geofizicheskiy Zhurnal Copyright (c) 2020 Геофизический журнал Copyright (c) 2020 Геофізичний журнал http://creativecommons.org/licenses/by/4.0 CC-BY Geofizicheskiy Zhurnal; Том 38, № 6 (2016); 118-136 Геофизический журнал; Том 38, № 6 (2016); 118-136 Геофізичний журнал; Том 38, № 6 (2016); 118-136 2524-1052 0203-3100 tectonics of the continental and oceanic plates thermodynamics crust mantle evolution of geosphere powers of mobilism elliptical orbit of the Earth gravity sole plates earthquakes continental drift fold system mid-ocean rifts info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2016 fturanojs 2020-10-12T23:28:52Z Based on thermodynamic analysis of the geological structure, PT conditions on the earth's surface, and the powers that cause tectonic drift of continental and oceanic plates, presented physical and chemical regularity of evolution geospheres. These mainly related to the space powers of the Earth rotation around its axis, by gravity powers of plates by the Earth, Sun and Moon, as well as between neighbors plates. In equatorial latitudes the rotational power is maximal and shift plates toward the equator. The most stable continent is Africa, which is associated with the maximum gravity to the Sun at perihelion elliptical orbit of the Earth. So, the drift of plates on the Earth's surface comes from Africa to the Pacific Ocean. Plate tectonics is primarily dependent on the plasticity of their base, which were magmatic in Archean and since Phanerozoic cooled with the formation plastic talc-serpentine soles. Due to which activated mobilism of plate. To the borders confined earthquake plates, which indicate the latter. Moving sedimentation zone during evolution transformed into folding system, which is much smaller in area, which is also indicate of plate tectonics. Oceanic plates have a small power, but significant temperature graditent, because in them since Mesozoic from ultramafic mantle melted basalt magma, which contributes to oceanic plates drift on the base of the magma and the continental plates on the talc-serpentine soles from the mid-ocean rifts. So open up the Atlantic and Indian oceans, and closes the Pacific. On Mars, we have been active in the Precambrian moving plates like Earth, which are mainly located in the equatorial zone, including the plate in the South pole Article in Journal/Newspaper South pole Scientific Periodicals of Ukraine (Ukrainian Research and Academic Network) Pacific Indian South Pole |
institution |
Open Polar |
collection |
Scientific Periodicals of Ukraine (Ukrainian Research and Academic Network) |
op_collection_id |
fturanojs |
language |
Russian |
topic |
tectonics of the continental and oceanic plates thermodynamics crust mantle evolution of geosphere powers of mobilism elliptical orbit of the Earth gravity sole plates earthquakes continental drift fold system mid-ocean rifts |
spellingShingle |
tectonics of the continental and oceanic plates thermodynamics crust mantle evolution of geosphere powers of mobilism elliptical orbit of the Earth gravity sole plates earthquakes continental drift fold system mid-ocean rifts Belevtsev, R.Ya. Blajko, V.I. Terechenko, S.I. About thermodynamic evolution of Еarth crust and tectonic plates |
topic_facet |
tectonics of the continental and oceanic plates thermodynamics crust mantle evolution of geosphere powers of mobilism elliptical orbit of the Earth gravity sole plates earthquakes continental drift fold system mid-ocean rifts |
description |
Based on thermodynamic analysis of the geological structure, PT conditions on the earth's surface, and the powers that cause tectonic drift of continental and oceanic plates, presented physical and chemical regularity of evolution geospheres. These mainly related to the space powers of the Earth rotation around its axis, by gravity powers of plates by the Earth, Sun and Moon, as well as between neighbors plates. In equatorial latitudes the rotational power is maximal and shift plates toward the equator. The most stable continent is Africa, which is associated with the maximum gravity to the Sun at perihelion elliptical orbit of the Earth. So, the drift of plates on the Earth's surface comes from Africa to the Pacific Ocean. Plate tectonics is primarily dependent on the plasticity of their base, which were magmatic in Archean and since Phanerozoic cooled with the formation plastic talc-serpentine soles. Due to which activated mobilism of plate. To the borders confined earthquake plates, which indicate the latter. Moving sedimentation zone during evolution transformed into folding system, which is much smaller in area, which is also indicate of plate tectonics. Oceanic plates have a small power, but significant temperature graditent, because in them since Mesozoic from ultramafic mantle melted basalt magma, which contributes to oceanic plates drift on the base of the magma and the continental plates on the talc-serpentine soles from the mid-ocean rifts. So open up the Atlantic and Indian oceans, and closes the Pacific. On Mars, we have been active in the Precambrian moving plates like Earth, which are mainly located in the equatorial zone, including the plate in the South pole |
format |
Article in Journal/Newspaper |
author |
Belevtsev, R.Ya. Blajko, V.I. Terechenko, S.I. |
author_facet |
Belevtsev, R.Ya. Blajko, V.I. Terechenko, S.I. |
author_sort |
Belevtsev, R.Ya. |
title |
About thermodynamic evolution of Еarth crust and tectonic plates |
title_short |
About thermodynamic evolution of Еarth crust and tectonic plates |
title_full |
About thermodynamic evolution of Еarth crust and tectonic plates |
title_fullStr |
About thermodynamic evolution of Еarth crust and tectonic plates |
title_full_unstemmed |
About thermodynamic evolution of Еarth crust and tectonic plates |
title_sort |
about thermodynamic evolution of еarth crust and tectonic plates |
publisher |
Subbotin Institute of Geophysics of the NAS of Ukraine |
publishDate |
2016 |
url |
http://journals.uran.ua/geofizicheskiy/article/view/91900 |
geographic |
Pacific Indian South Pole |
geographic_facet |
Pacific Indian South Pole |
genre |
South pole |
genre_facet |
South pole |
op_source |
Geofizicheskiy Zhurnal; Том 38, № 6 (2016); 118-136 Геофизический журнал; Том 38, № 6 (2016); 118-136 Геофізичний журнал; Том 38, № 6 (2016); 118-136 2524-1052 0203-3100 |
op_relation |
http://journals.uran.ua/geofizicheskiy/article/view/91900/87678 http://journals.uran.ua/geofizicheskiy/article/view/91900 |
op_rights |
Copyright (c) 2020 Geofizicheskiy Zhurnal Copyright (c) 2020 Геофизический журнал Copyright (c) 2020 Геофізичний журнал http://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
_version_ |
1766202743988420608 |