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Paleogeographic settings and tectonic deformations of the Barents Sea continental margin in the Cenozoic

Paleogeographic settings and tectonic deformations of the Barents Sea continental margin in the... ISSN 1028-334X, Doklady Earth Scices, 2006, Vol. 407A, No. 3, pp. 366–371. © Pleiades Publishing, Inc., 2006. Original Russian Text © E.V. Shipilov, V.A. Tyuremnov, V.N. Glaznev, V.A. Golubev, 2006, published in Doklady Akademii Nauk, 2006, Vol. 407, No. 3, pp. 378–383. GEOLOGY E. V. Shipilov1, V. A. Tyuremnov2, V. N. Glaznev2, and V. A. Golubev1 Prested by Academician G. G. Matishov June 2, 2005 Received June 29, 2005 DOI: 10.1134/S1028334X06030056 The Bar Sea contintal margin (hereafter, Bar margin) differs from other passive margins by the most exive shelf, the giant thickness of sedimtary rocks in basins and troughs, and i unique tectonic position. The outer, almost rectangular promontory of the Bar margin ju out into i deepwater western and northern framing (Fig. 1), idtified as the Norwegian–Greland and Eurasia basins, respectively. In this regard, the contintal margin is affected by two, mutually perpdicular spreading zones (Knipovich and Gakkel ridges). The evolution of oceanic basins proceeded in the course of continuous tectonic and geodynamic interaction with the framing contintal margins. In our case, this was expressed, first of all, in the separation and evolution of the Bar Sea shelf platform as an area of neotectonic transformations during the http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Doklady Earth Sciences Springer Journals

Paleogeographic settings and tectonic deformations of the Barents Sea continental margin in the Cenozoic

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References (1)

Publisher
Springer Journals
Copyright
Copyright © 2006 by Nauka/Interperiodica
Subject
Earth Sciences; Earth Sciences, general
ISSN
1028-334X
eISSN
1531-8354
DOI
10.1134/S1028334X06030056
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Abstract

ISSN 1028-334X, Doklady Earth Scices, 2006, Vol. 407A, No. 3, pp. 366–371. © Pleiades Publishing, Inc., 2006. Original Russian Text © E.V. Shipilov, V.A. Tyuremnov, V.N. Glaznev, V.A. Golubev, 2006, published in Doklady Akademii Nauk, 2006, Vol. 407, No. 3, pp. 378–383. GEOLOGY E. V. Shipilov1, V. A. Tyuremnov2, V. N. Glaznev2, and V. A. Golubev1 Prested by Academician G. G. Matishov June 2, 2005 Received June 29, 2005 DOI: 10.1134/S1028334X06030056 The Bar Sea contintal margin (hereafter, Bar margin) differs from other passive margins by the most exive shelf, the giant thickness of sedimtary rocks in basins and troughs, and i unique tectonic position. The outer, almost rectangular promontory of the Bar margin ju out into i deepwater western and northern framing (Fig. 1), idtified as the Norwegian–Greland and Eurasia basins, respectively. In this regard, the contintal margin is affected by two, mutually perpdicular spreading zones (Knipovich and Gakkel ridges). The evolution of oceanic basins proceeded in the course of continuous tectonic and geodynamic interaction with the framing contintal margins. In our case, this was expressed, first of all, in the separation and evolution of the Bar Sea shelf platform as an area of neotectonic transformations during the

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Doklady Earth Sciences – Springer Journals

Published: Mar 1, 2006

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