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New data on the geological structure of the junction between the Cape Verde Seamount and the Cape Verde Basin, central Atlantic

New data on the geological structure of the junction between the Cape Verde Seamount and the Cape... ISSN 1028-334X, Doklady Earth Sciences, 2006, Vol. 407, No. 2, pp. 220–224. © Pleiades Publishing, Inc., 2006. Original Russian Text © S.G. Skolotnev, A.A. Peive, N.N. Turko, N.V. Tsukanov, L.A. Golovina, V.N. Efimov, A.E. Eskin, V.Yu. Lavrushin, V.V. Petrova, N.L. Chaplygina, 2006, published in Doklady Akademii Nauk, 2006, Vol. 407, No. 2, pp. 224–229. GEOLOGY S. G. Skolotnev, A. A. Peive, N. N. Turko, N. V. Tsukanov, L. A. Golovina, V. N. Efimov, A. E. Eskin, V. Yu. Lavrushin, V. V. Petrova, and N. L. Chaplygina Presented by Academician Yu. M. Pushcharovsky August 25, 2005 Received September 1, 2005 DOI: 10.1134/S1028334X06020140 The regions of conjugation of continental rise with abyssal oceanic basins at the margins of the Atlantic— a transitional zone between continental and oceanic lithospheres—are still poorly studied in geological terms. In the course of expeditions conducted by the Geological Institute (Moscow), the structure of this zone was studied at the continental slope of Africa, south of the Cape Verde Islands. In this area, the continental rise widens sharply making up a near-latitudinal promontory that divides the abyssal Cape Verde Basin in the south and the Canary Basin in the north. The study area is situated in http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Doklady Earth Sciences Springer Journals

New data on the geological structure of the junction between the Cape Verde Seamount and the Cape Verde Basin, central Atlantic

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References (2)

Publisher
Springer Journals
Copyright
Copyright © 2006 by Nauka/Interperiodica
Subject
Earth Sciences; Earth Sciences, general
ISSN
1028-334X
eISSN
1531-8354
DOI
10.1134/S1028334X06020140
Publisher site
See Article on Publisher Site

Abstract

ISSN 1028-334X, Doklady Earth Sciences, 2006, Vol. 407, No. 2, pp. 220–224. © Pleiades Publishing, Inc., 2006. Original Russian Text © S.G. Skolotnev, A.A. Peive, N.N. Turko, N.V. Tsukanov, L.A. Golovina, V.N. Efimov, A.E. Eskin, V.Yu. Lavrushin, V.V. Petrova, N.L. Chaplygina, 2006, published in Doklady Akademii Nauk, 2006, Vol. 407, No. 2, pp. 224–229. GEOLOGY S. G. Skolotnev, A. A. Peive, N. N. Turko, N. V. Tsukanov, L. A. Golovina, V. N. Efimov, A. E. Eskin, V. Yu. Lavrushin, V. V. Petrova, and N. L. Chaplygina Presented by Academician Yu. M. Pushcharovsky August 25, 2005 Received September 1, 2005 DOI: 10.1134/S1028334X06020140 The regions of conjugation of continental rise with abyssal oceanic basins at the margins of the Atlantic— a transitional zone between continental and oceanic lithospheres—are still poorly studied in geological terms. In the course of expeditions conducted by the Geological Institute (Moscow), the structure of this zone was studied at the continental slope of Africa, south of the Cape Verde Islands. In this area, the continental rise widens sharply making up a near-latitudinal promontory that divides the abyssal Cape Verde Basin in the south and the Canary Basin in the north. The study area is situated in

Journal

Doklady Earth SciencesSpringer Journals

Published: Feb 1, 2006

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