Standard

Methods and results of processing of complex seismic investigations on the 2-AR profile (Barents-Kara Shelf). / Sakulina, T. S.; Roslov, Yu V.; Pavlenkova, G. A.

в: Izvestiya, Physics of the Solid Earth, Том 45, № 3, 2009, стр. 231-238.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Sakulina, TS, Roslov, YV & Pavlenkova, GA 2009, 'Methods and results of processing of complex seismic investigations on the 2-AR profile (Barents-Kara Shelf)', Izvestiya, Physics of the Solid Earth, Том. 45, № 3, стр. 231-238. https://doi.org/10.1134/S1069351309030045

APA

Sakulina, T. S., Roslov, Y. V., & Pavlenkova, G. A. (2009). Methods and results of processing of complex seismic investigations on the 2-AR profile (Barents-Kara Shelf). Izvestiya, Physics of the Solid Earth, 45(3), 231-238. https://doi.org/10.1134/S1069351309030045

Vancouver

Sakulina TS, Roslov YV, Pavlenkova GA. Methods and results of processing of complex seismic investigations on the 2-AR profile (Barents-Kara Shelf). Izvestiya, Physics of the Solid Earth. 2009;45(3):231-238. https://doi.org/10.1134/S1069351309030045

Author

Sakulina, T. S. ; Roslov, Yu V. ; Pavlenkova, G. A. / Methods and results of processing of complex seismic investigations on the 2-AR profile (Barents-Kara Shelf). в: Izvestiya, Physics of the Solid Earth. 2009 ; Том 45, № 3. стр. 231-238.

BibTeX

@article{1345136338564477979cef2a9f14bcb0,
title = "Methods and results of processing of complex seismic investigations on the 2-AR profile (Barents-Kara Shelf)",
abstract = "Extensive seismic investigations of the crust and upper mantle have been carried out in the region of the Barents and Kara seas during the past decade. One of the profiles (2-AR) measured by FGU NPP {"}Sevmorgeo{"} with the CDP and deep seismic sounding methods was successfully used for comparatively analyzing different technologies of constructing seismic sections and for demonstrating a high information content of the method of mathematical modeling and the constructions of wave sections from supercritical reflected waves. It is shown that the crusts of the North Barents and South Kara basins are different. In the first case, the velocity section changes insignificantly, whereas, in the second case, velocities in the crust increase under the basin and the M boundary rises. The crust of the Novaya Zemlya orogen has a thickness of 48 km, and its average thickness on the profile is 35 km.",
author = "Sakulina, {T. S.} and Roslov, {Yu V.} and Pavlenkova, {G. A.}",
note = "Copyright: Copyright 2009 Elsevier B.V., All rights reserved.",
year = "2009",
doi = "10.1134/S1069351309030045",
language = "English",
volume = "45",
pages = "231--238",
journal = "Izvestiya, Physics of the Solid Earth",
issn = "1069-3513",
publisher = "Pleiades Publishing",
number = "3",

}

RIS

TY - JOUR

T1 - Methods and results of processing of complex seismic investigations on the 2-AR profile (Barents-Kara Shelf)

AU - Sakulina, T. S.

AU - Roslov, Yu V.

AU - Pavlenkova, G. A.

N1 - Copyright: Copyright 2009 Elsevier B.V., All rights reserved.

PY - 2009

Y1 - 2009

N2 - Extensive seismic investigations of the crust and upper mantle have been carried out in the region of the Barents and Kara seas during the past decade. One of the profiles (2-AR) measured by FGU NPP "Sevmorgeo" with the CDP and deep seismic sounding methods was successfully used for comparatively analyzing different technologies of constructing seismic sections and for demonstrating a high information content of the method of mathematical modeling and the constructions of wave sections from supercritical reflected waves. It is shown that the crusts of the North Barents and South Kara basins are different. In the first case, the velocity section changes insignificantly, whereas, in the second case, velocities in the crust increase under the basin and the M boundary rises. The crust of the Novaya Zemlya orogen has a thickness of 48 km, and its average thickness on the profile is 35 km.

AB - Extensive seismic investigations of the crust and upper mantle have been carried out in the region of the Barents and Kara seas during the past decade. One of the profiles (2-AR) measured by FGU NPP "Sevmorgeo" with the CDP and deep seismic sounding methods was successfully used for comparatively analyzing different technologies of constructing seismic sections and for demonstrating a high information content of the method of mathematical modeling and the constructions of wave sections from supercritical reflected waves. It is shown that the crusts of the North Barents and South Kara basins are different. In the first case, the velocity section changes insignificantly, whereas, in the second case, velocities in the crust increase under the basin and the M boundary rises. The crust of the Novaya Zemlya orogen has a thickness of 48 km, and its average thickness on the profile is 35 km.

UR - http://www.scopus.com/inward/record.url?scp=62649174652&partnerID=8YFLogxK

U2 - 10.1134/S1069351309030045

DO - 10.1134/S1069351309030045

M3 - Article

AN - SCOPUS:62649174652

VL - 45

SP - 231

EP - 238

JO - Izvestiya, Physics of the Solid Earth

JF - Izvestiya, Physics of the Solid Earth

SN - 1069-3513

IS - 3

ER -

ID: 78169218