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Hauptverfasser: Kurentsova, Natalia A, Udintsev, Gleb B
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2004
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Online-Zugang:https://doi.org/10.1594/PANGAEA.783702
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author Kurentsova, Natalia A
Udintsev, Gleb B
author_facet Kurentsova, Natalia A
Udintsev, Gleb B
collection Datos científicos de ciencias marinas y ambientales
contents 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 Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_783702
institution PANGAEA
language en
publishDate 2004
publisher PANGAEA
record_format pangaea
spellingShingle Chemial and isotope compositions of rocks from the West Antarctic
Kurentsova, Natalia A
Udintsev, Gleb B
AIPS; Antarctic; Archive of Ocean Data; ARCOD; BGr-10; D1; D2; D3; DiRi; Dn34-2; Dn35-1; GI; HB; MULT; Multiple investigations; SIS; SMIS
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.
title Chemial and isotope compositions of rocks from the West Antarctic
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
url https://doi.org/10.1594/PANGAEA.783702