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 Ear...
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| Datum: | 2016 |
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S. Subbotin Institute of Geophysics of the NAS of Ukraine
2016
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| Online Zugang: | https://journals.uran.ua/geofizicheskiy/article/view/91900 |
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| Назва журналу: | Geofizicheskiy Zhurnal |
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Geofizicheskiy Zhurnal| _version_ | 1856543113632284672 |
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| 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. |
| baseUrl_str | |
| collection | OJS |
| datestamp_date | 2020-10-07T11:18:21Z |
| 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 |
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| format | Article |
| id | journalsuranua-geofizicheskiy-article-91900 |
| institution | Geofizicheskiy Zhurnal |
| language | Russian |
| last_indexed | 2025-07-17T11:04:39Z |
| publishDate | 2016 |
| publisher | S. Subbotin Institute of Geophysics of the NAS of Ukraine |
| record_format | ojs |
| spelling | journalsuranua-geofizicheskiy-article-919002020-10-07T11:18:21Z About thermodynamic evolution of Еarth crust and tectonic plates Belevtsev, R.Ya. Blajko, V.I. Terechenko, S.I. 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 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 S. Subbotin Institute of Geophysics of the NAS of Ukraine 2016-12-01 Article Article application/pdf https://journals.uran.ua/geofizicheskiy/article/view/91900 10.24028/gzh.0203-3100.v38i6.2016.91900 Geofizicheskiy Zhurnal; Vol. 38 No. 6 (2016); 118-136 Геофизический журнал; Том 38 № 6 (2016); 118-136 Геофізичний журнал; Том 38 № 6 (2016); 118-136 2524-1052 0203-3100 ru https://journals.uran.ua/geofizicheskiy/article/view/91900/87678 Copyright (c) 2020 Geofizicheskiy Zhurnal https://creativecommons.org/licenses/by/4.0 |
| 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 |
| title | 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_short | About thermodynamic evolution of Еarth crust and tectonic plates |
| title_sort | about thermodynamic evolution of еarth crust and tectonic plates |
| 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 |
| 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 |
| url | https://journals.uran.ua/geofizicheskiy/article/view/91900 |
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