Chemial and isotope compositions of rocks from the West Antarctic
The paper is devoted to a marine geophysical-geological research in the West Antarctic. This researche contributed to establishing the base geodesic network of the West Antarctic and supplemented geokinematic monitoring based on this network with geophysical and geologic information on structure and...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.783702 2023-05-15T13:42:10+02:00 Chemial and isotope compositions of rocks from the West Antarctic Kurentsova, Natalia A Udintsev, Gleb B MEDIAN LATITUDE: -60.823645 * MEDIAN LONGITUDE: -46.321689 * SOUTH-BOUND LATITUDE: -68.850000 * WEST-BOUND LONGITUDE: -90.750000 * NORTH-BOUND LATITUDE: -56.400000 * EAST-BOUND LONGITUDE: -26.700000 2004-06-06 application/zip, 6 datasets https://doi.pangaea.de/10.1594/PANGAEA.783702 https://doi.org/10.1594/PANGAEA.783702 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.783702 https://doi.org/10.1594/PANGAEA.783702 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Moscow Supplement to: Kurentsova, Natalia A; Udintsev, Gleb B (2004): The main features of the structure and evolution of the southern part of the Scotia Sea, West Antarctic. Tikhookeanskaya Geologiya (Pacific Geology), 23(5), 25-39 AIPS Antarctic Archive of Ocean Data ARCOD BGr-10 D1 D2 D3 DiRi Dn34-2 Dn35-1 GI HB MULT Multiple investigations SIS SMIS Dataset 2004 ftpangaea https://doi.org/10.1594/PANGAEA.783702 2023-01-20T07:32:34Z The paper is devoted to a marine geophysical-geological research in the West Antarctic. This researche contributed to establishing the base geodesic network of the West Antarctic and supplemented geokinematic monitoring based on this network with geophysical and geologic information on structure and features of geomorphological and tectonic development of the South Ocean floor. Collected materials allow to conclude about the inhomogeneity of the Scotia Sea floor and about combination of fragments of a continental massif with young rift structures in conditions of the upwelling mantle. The ancient continental bridge, faunal connections between the South America and the West Antarctic has been destroyed by processes of destruction, taphrogeny and sea floor spreading. Structures of the Scotia and Caribbean Seas, North Fiji and Arctic Basins are similar. Dataset Antarc* Antarctic Arctic Scotia Sea PANGAEA - Data Publisher for Earth & Environmental Science Arctic Antarctic Scotia Sea ENVELOPE(-90.750000,-26.700000,-56.400000,-68.850000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
AIPS Antarctic Archive of Ocean Data ARCOD BGr-10 D1 D2 D3 DiRi Dn34-2 Dn35-1 GI HB MULT Multiple investigations SIS SMIS |
spellingShingle |
AIPS Antarctic Archive of Ocean Data ARCOD BGr-10 D1 D2 D3 DiRi Dn34-2 Dn35-1 GI HB MULT Multiple investigations SIS SMIS Kurentsova, Natalia A Udintsev, Gleb B Chemial and isotope compositions of rocks from the West Antarctic |
topic_facet |
AIPS Antarctic Archive of Ocean Data ARCOD BGr-10 D1 D2 D3 DiRi Dn34-2 Dn35-1 GI HB MULT Multiple investigations SIS SMIS |
description |
The paper is devoted to a marine geophysical-geological research in the West Antarctic. This researche contributed to establishing the base geodesic network of the West Antarctic and supplemented geokinematic monitoring based on this network with geophysical and geologic information on structure and features of geomorphological and tectonic development of the South Ocean floor. Collected materials allow to conclude about the inhomogeneity of the Scotia Sea floor and about combination of fragments of a continental massif with young rift structures in conditions of the upwelling mantle. The ancient continental bridge, faunal connections between the South America and the West Antarctic has been destroyed by processes of destruction, taphrogeny and sea floor spreading. Structures of the Scotia and Caribbean Seas, North Fiji and Arctic Basins are similar. |
format |
Dataset |
author |
Kurentsova, Natalia A Udintsev, Gleb B |
author_facet |
Kurentsova, Natalia A Udintsev, Gleb B |
author_sort |
Kurentsova, Natalia A |
title |
Chemial and isotope compositions of rocks from the West Antarctic |
title_short |
Chemial and isotope compositions of rocks from the West Antarctic |
title_full |
Chemial and isotope compositions of rocks from the West Antarctic |
title_fullStr |
Chemial and isotope compositions of rocks from the West Antarctic |
title_full_unstemmed |
Chemial and isotope compositions of rocks from the West Antarctic |
title_sort |
chemial and isotope compositions of rocks from the west antarctic |
publisher |
PANGAEA |
publishDate |
2004 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.783702 https://doi.org/10.1594/PANGAEA.783702 |
op_coverage |
MEDIAN LATITUDE: -60.823645 * MEDIAN LONGITUDE: -46.321689 * SOUTH-BOUND LATITUDE: -68.850000 * WEST-BOUND LONGITUDE: -90.750000 * NORTH-BOUND LATITUDE: -56.400000 * EAST-BOUND LONGITUDE: -26.700000 |
long_lat |
ENVELOPE(-90.750000,-26.700000,-56.400000,-68.850000) |
geographic |
Arctic Antarctic Scotia Sea |
geographic_facet |
Arctic Antarctic Scotia Sea |
genre |
Antarc* Antarctic Arctic Scotia Sea |
genre_facet |
Antarc* Antarctic Arctic Scotia Sea |
op_source |
V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Moscow Supplement to: Kurentsova, Natalia A; Udintsev, Gleb B (2004): The main features of the structure and evolution of the southern part of the Scotia Sea, West Antarctic. Tikhookeanskaya Geologiya (Pacific Geology), 23(5), 25-39 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.783702 https://doi.org/10.1594/PANGAEA.783702 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.783702 |
_version_ |
1766164256298893312 |