A new astrobleme in the Pacific Ocean

A new astrobleme in the Pacific Ocean ISSN 1028-334X, Doklady Earth Sciences, 2006, Vol. 411, No. 8, pp. 1336–1338. © Pleiades Publishing, Inc., 2006. Original Russian Text © B.W. Levin, E.V. Gretskaya, G.S. Nemchenko, 2006, published in Doklady Akademii Nauk, 2006, Vol. 411, No. 2, pp. 259–261. OCEANOLOGY A New Astrobleme in the Pacific Ocean1 Corresponding Member of RAS B. W. Levin, E. V. Gretskaya, and G. S. Nemchenko Received May 10, 2006 DOI: 10.1134/S1028334X06080381 30° 1 This article was translated by the authors. 169°30′ Institute of Marine Geology and Geophysics, Far East Division, Russian Academy of Sciences, ul. Nauki 2, Yuzhno-Sakhalinsk, 693002 Russia 1336 170° E Fig. 1. Scheme of CSP profiles at the test site. Dashed line shows the 5900-m isobath. Recent decades have been characterized by great interest in study of ring structures formed as a result of falling cosmic bodies [1]. Of all similar structures, astroblemes found on the ocean floor are of special interest. The small number of them is explained by the difficulty of finding them and poor study of the ocean. Generally, such structures are revealed by chance as not corresponding to the general tectonic plan. The ring structure in the Northwestern Pacific was discovered by Sakhalin researchers http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Doklady Earth Sciences Springer Journals

A new astrobleme in the Pacific Ocean

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Publisher
Springer Journals
Copyright
Copyright © 2006 by Nauka/Interperiodica
Subject
Earth Sciences; Earth Sciences, general
ISSN
1028-334X
eISSN
1531-8354
D.O.I.
10.1134/S1028334X06080381
Publisher site
See Article on Publisher Site

Abstract

ISSN 1028-334X, Doklady Earth Sciences, 2006, Vol. 411, No. 8, pp. 1336–1338. © Pleiades Publishing, Inc., 2006. Original Russian Text © B.W. Levin, E.V. Gretskaya, G.S. Nemchenko, 2006, published in Doklady Akademii Nauk, 2006, Vol. 411, No. 2, pp. 259–261. OCEANOLOGY A New Astrobleme in the Pacific Ocean1 Corresponding Member of RAS B. W. Levin, E. V. Gretskaya, and G. S. Nemchenko Received May 10, 2006 DOI: 10.1134/S1028334X06080381 30° 1 This article was translated by the authors. 169°30′ Institute of Marine Geology and Geophysics, Far East Division, Russian Academy of Sciences, ul. Nauki 2, Yuzhno-Sakhalinsk, 693002 Russia 1336 170° E Fig. 1. Scheme of CSP profiles at the test site. Dashed line shows the 5900-m isobath. Recent decades have been characterized by great interest in study of ring structures formed as a result of falling cosmic bodies [1]. Of all similar structures, astroblemes found on the ocean floor are of special interest. The small number of them is explained by the difficulty of finding them and poor study of the ocean. Generally, such structures are revealed by chance as not corresponding to the general tectonic plan. The ring structure in the Northwestern Pacific was discovered by Sakhalin researchers

Journal

Doklady Earth SciencesSpringer Journals

Published: Nov 1, 2006

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