Строение и история развития литосферы - стр. 127
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A. V. Zayonchek[81], H. Brekke[82], S. Yu. Sokolov[83], A.O. Mazarovich[84], K.O. Dobrolyubova[85], V. N. Efimov[86], A. S. Abramova[87], Yu. A. Zaraiskaya[88], A.V. Kokhan[89], E. A. Moroz[90], A. A. Peive[91], N.P. Chamov[92], K. P. Yampol’skii[93]. The Structure of Continent-Ocean transition zone at North-West Barents Sea Margin (results of 24–26-th cruises of RV «Akademik Nikolaj Strakhov», 2006–2009)
Abstract
Three geological-geophysical expeditions on R/V «Akademik Nikolaj Strakhov» in 2006–2009 (Geological Institute RAS, Norwegian Petroleum Directorate) resulted in detailed mapping by acoustic methods for significant areas of Knipovich ridge, southern slope of Mohn ridge, Storfjord and Orli troughs, continental slope and Franz-Joseph Land vicinity with total survey length about 22 000 km. Were discovered: northward zone of Svalbard shelf plate destruction, outcrops of dyke complexes and other volcanogeneous edifices on the shelf, gas hydrates release occurrences, modern tectonic displacements on continental slope and in sedimentary cover of Knipovich and Mohn ridges boards and many other facts. North-West margin of Barents sea shelf exposes the similarity with rift onshore structures at Northern areas of Spitzbergen Island, that could show the uniform conditions of their formation, and with the consideration of the data from neighbors areas at deep ocean gives the basis for development of model, connecting the geodynamic processes at continental and oceanic lithosphere.