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ISSN 1028-334X, Doklady Earth Sciences, 2006, Vol. 407, No. 2, pp. 220â224. © Pleiades Publishing, Inc., 2006. Original Russian Text © S.G. Skolotnev, A.A. Peive, N.N. Turko, N.V. Tsukanov, L.A. Golovina, V.N. Eï¬mov, A.E. Eskin, V.Yu. Lavrushin, V.V. Petrova, N.L. Chaplygina, 2006, published in Doklady Akademii Nauk, 2006, Vol. 407, No. 2, pp. 224â229. 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 Atlanticâ a transitional zone between continental and oceanic lithospheresâare 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
Doklady Earth Sciences – Springer Journals
Published: Feb 1, 2006
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