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Depth model of the Barents and Kara seas according to geophysical surveys results

By
N. M. Ivanova
N. M. Ivanova
Sevmorgeo, Rosenshtein str. 36, St Petersburg, Russia
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T. S. Sakulina
T. S. Sakulina
Sevmorgeo, Rosenshtein str. 36, St Petersburg, Russia
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I. V. Belyaev
I. V. Belyaev
Sevmorgeo, Rosenshtein str. 36, St Petersburg, Russia
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Yu. I. Matveev
Yu. I. Matveev
Sevmorgeo, Rosenshtein str. 36, St Petersburg, Russia
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Yu. V. Roslov
Yu. V. Roslov
Sevmorgeo, Rosenshtein str. 36, St Petersburg, Russia
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Published:
January 01, 2011

Abstract

In 1995–2006 FSUE ‘Sevmorgeo’ within the framework of the Federal Program of state survey baselines network development performed geophysical works in the Barents and Kara seas along four regional profiles: 1-AR (Kola Peninsula–Heysa Island of Franz-Joseph Land Archipelago); 2-AR (Central part of the Barents region–Novaya Zemlya – Yamal Peninsula); 3-AR (White Sea–Severnaya Zemlya Archipelago); and 4-AR (Taimyr Peninsula–Franz-Joseph Land Archipelago). Geophysical surveys included works using seismic refraction–deep seismic sounding technique, seismic reflection–common-depth point technique, seismic acoustic profiling and gravimetric and magnetic measurements. Integrated geophysical surveys along the regional profiles enabled more exact definition of the Earth deep crustal structure and the sedimentary cover of the main tectonic elements.

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Contents

Geological Society, London, Memoirs

Arctic Petroleum Geology

Anthony M. Spencer
Anthony M. Spencer
Statoil, Norway
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Ashton F. Embry
Ashton F. Embry
Geological Survey of Canada, Canada
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Donald L. Gautier
Donald L. Gautier
United States Geological Survey, USA
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Antonina V. Stoupakova
Antonina V. Stoupakova
Moscow State University, Russia
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Kai Sørensen
Kai Sørensen
Geological Survey of Denmark and Greenland
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Geological Society of London
Volume
35
ISBN electronic:
9781862394100
Publication date:
January 01, 2011

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