Tectonosphere and formation of the Mozambique Ridge: density and physical modeling
The tectonosphere and formation conditions of the Mozambique Ridge are considered. The Mozambique Ridge is located in the southwestern part of the Indian Ocean between the Natal and the Mozambique Mesozoic Basins. The way how the ridge formed remains debatable. The anomalous structure of the crust o...
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Institute of Volcanology and Seismology FEB RAS
2022
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ftdoajarticles:oai:doaj.org/article:8850b46f93454e99b05b4c4ec3e6d577 2023-05-15T13:57:36+02:00 Tectonosphere and formation of the Mozambique Ridge: density and physical modeling Ryzhova D.A. Tolstova A.I. Dubinin E.P. Kosnyreva M.V. Bulychev A.A. Grokholsky A.L. 2022-04-01T00:00:00Z https://doi.org/10.31431/1816-5524-2022-1-53-46-58 https://doaj.org/article/8850b46f93454e99b05b4c4ec3e6d577 RU rus Institute of Volcanology and Seismology FEB RAS http://www.kscnet.ru/journal/kraesc/article/view/703 https://doaj.org/toc/1816-5524 https://doaj.org/toc/1816-5532 1816-5524 1816-5532 doi:10.31431/1816-5524-2022-1-53-46-58 https://doaj.org/article/8850b46f93454e99b05b4c4ec3e6d577 Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле, Vol 53, Iss 1, Pp 46-58 (2022) mozambique ridge tectonosphere spreading density and physical modeling Geology QE1-996.5 article 2022 ftdoajarticles https://doi.org/10.31431/1816-5524-2022-1-53-46-58 2022-12-31T04:36:29Z The tectonosphere and formation conditions of the Mozambique Ridge are considered. The Mozambique Ridge is located in the southwestern part of the Indian Ocean between the Natal and the Mozambique Mesozoic Basins. The way how the ridge formed remains debatable. The anomalous structure of the crust of the Mozambique Ridge can be explained either by underplaying - thickening of the oceanic crust from below due to magmatism, or by stretching and thinning of the continental crust. Based on gravitational and magnetic field anomalies, seismotomography and other geological and geophysical information, density modeling was carried out along four profiles. Physical modeling determined the conditions of formation of the Mozambique Ridge. It formed due to the splitting of the African-Antarctic continent, the presence of structural heterogeneities in the lithosphere of the African continent and the influence of the Karoo plume. Article in Journal/Newspaper Antarc* Antarctic Directory of Open Access Journals: DOAJ Articles Antarctic Indian BULLETIN OF KAMCHATKA REGIONAL ASSOCIATION «EDUCATIONAL-SCIENTIFIC CENTER». EARTH SCIENCES 1 53 46 58 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
Russian |
topic |
mozambique ridge tectonosphere spreading density and physical modeling Geology QE1-996.5 |
spellingShingle |
mozambique ridge tectonosphere spreading density and physical modeling Geology QE1-996.5 Ryzhova D.A. Tolstova A.I. Dubinin E.P. Kosnyreva M.V. Bulychev A.A. Grokholsky A.L. Tectonosphere and formation of the Mozambique Ridge: density and physical modeling |
topic_facet |
mozambique ridge tectonosphere spreading density and physical modeling Geology QE1-996.5 |
description |
The tectonosphere and formation conditions of the Mozambique Ridge are considered. The Mozambique Ridge is located in the southwestern part of the Indian Ocean between the Natal and the Mozambique Mesozoic Basins. The way how the ridge formed remains debatable. The anomalous structure of the crust of the Mozambique Ridge can be explained either by underplaying - thickening of the oceanic crust from below due to magmatism, or by stretching and thinning of the continental crust. Based on gravitational and magnetic field anomalies, seismotomography and other geological and geophysical information, density modeling was carried out along four profiles. Physical modeling determined the conditions of formation of the Mozambique Ridge. It formed due to the splitting of the African-Antarctic continent, the presence of structural heterogeneities in the lithosphere of the African continent and the influence of the Karoo plume. |
format |
Article in Journal/Newspaper |
author |
Ryzhova D.A. Tolstova A.I. Dubinin E.P. Kosnyreva M.V. Bulychev A.A. Grokholsky A.L. |
author_facet |
Ryzhova D.A. Tolstova A.I. Dubinin E.P. Kosnyreva M.V. Bulychev A.A. Grokholsky A.L. |
author_sort |
Ryzhova D.A. |
title |
Tectonosphere and formation of the Mozambique Ridge: density and physical modeling |
title_short |
Tectonosphere and formation of the Mozambique Ridge: density and physical modeling |
title_full |
Tectonosphere and formation of the Mozambique Ridge: density and physical modeling |
title_fullStr |
Tectonosphere and formation of the Mozambique Ridge: density and physical modeling |
title_full_unstemmed |
Tectonosphere and formation of the Mozambique Ridge: density and physical modeling |
title_sort |
tectonosphere and formation of the mozambique ridge: density and physical modeling |
publisher |
Institute of Volcanology and Seismology FEB RAS |
publishDate |
2022 |
url |
https://doi.org/10.31431/1816-5524-2022-1-53-46-58 https://doaj.org/article/8850b46f93454e99b05b4c4ec3e6d577 |
geographic |
Antarctic Indian |
geographic_facet |
Antarctic Indian |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
Вестник Камчатской региональной ассоциации "Учебно-научный центр". Серия: Науки о Земле, Vol 53, Iss 1, Pp 46-58 (2022) |
op_relation |
http://www.kscnet.ru/journal/kraesc/article/view/703 https://doaj.org/toc/1816-5524 https://doaj.org/toc/1816-5532 1816-5524 1816-5532 doi:10.31431/1816-5524-2022-1-53-46-58 https://doaj.org/article/8850b46f93454e99b05b4c4ec3e6d577 |
op_doi |
https://doi.org/10.31431/1816-5524-2022-1-53-46-58 |
container_title |
BULLETIN OF KAMCHATKA REGIONAL ASSOCIATION «EDUCATIONAL-SCIENTIFIC CENTER». EARTH SCIENCES |
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53 |
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