Standard

Deep structure of the crust beneath the Sea of Okhotsk inferred from 3D seismic density modeling. / Piskarev, A. L.; Butsenko, V. V.; Poselov, V. A.; Savin, V. A.

в: Oceanology, Том 52, № 3, 01.05.2012, стр. 411-421.

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

Harvard

Piskarev, AL, Butsenko, VV, Poselov, VA & Savin, VA 2012, 'Deep structure of the crust beneath the Sea of Okhotsk inferred from 3D seismic density modeling', Oceanology, Том. 52, № 3, стр. 411-421. https://doi.org/10.1134/S0001437012030095

APA

Piskarev, A. L., Butsenko, V. V., Poselov, V. A., & Savin, V. A. (2012). Deep structure of the crust beneath the Sea of Okhotsk inferred from 3D seismic density modeling. Oceanology, 52(3), 411-421. https://doi.org/10.1134/S0001437012030095

Vancouver

Piskarev AL, Butsenko VV, Poselov VA, Savin VA. Deep structure of the crust beneath the Sea of Okhotsk inferred from 3D seismic density modeling. Oceanology. 2012 Май 1;52(3):411-421. https://doi.org/10.1134/S0001437012030095

Author

Piskarev, A. L. ; Butsenko, V. V. ; Poselov, V. A. ; Savin, V. A. / Deep structure of the crust beneath the Sea of Okhotsk inferred from 3D seismic density modeling. в: Oceanology. 2012 ; Том 52, № 3. стр. 411-421.

BibTeX

@article{83bc285e9f334c3593c409208fec00e5,
title = "Deep structure of the crust beneath the Sea of Okhotsk inferred from 3D seismic density modeling",
abstract = "Potential field anomalies of the Sea of Okhotsk region are analyzed for compiling a map of the basement's tectonic structures. A 3D density model of the Earth's crust is constructed using seismogeological and experimental-petrophysical data, which made it possible to obtain a visual image of main structures of the region reflecting the observable geophysical anomalies. The obtained data allow a domain located in the central part of the Sea of Okhotsk beyond the limits of the exclusive economic zone of the Russian Federation to be considered as a natural continuation of the continental shelf since the latter is structurally similar to western Kamchatka. The deep structural boundaries rise beneath the large sedimentary Deryugin and Tinro basins, which is characteristic of petroliferous basins.",
author = "Piskarev, {A. L.} and Butsenko, {V. V.} and Poselov, {V. A.} and Savin, {V. A.}",
year = "2012",
month = may,
day = "1",
doi = "10.1134/S0001437012030095",
language = "English",
volume = "52",
pages = "411--421",
journal = "Oceanology",
issn = "0001-4370",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "3",

}

RIS

TY - JOUR

T1 - Deep structure of the crust beneath the Sea of Okhotsk inferred from 3D seismic density modeling

AU - Piskarev, A. L.

AU - Butsenko, V. V.

AU - Poselov, V. A.

AU - Savin, V. A.

PY - 2012/5/1

Y1 - 2012/5/1

N2 - Potential field anomalies of the Sea of Okhotsk region are analyzed for compiling a map of the basement's tectonic structures. A 3D density model of the Earth's crust is constructed using seismogeological and experimental-petrophysical data, which made it possible to obtain a visual image of main structures of the region reflecting the observable geophysical anomalies. The obtained data allow a domain located in the central part of the Sea of Okhotsk beyond the limits of the exclusive economic zone of the Russian Federation to be considered as a natural continuation of the continental shelf since the latter is structurally similar to western Kamchatka. The deep structural boundaries rise beneath the large sedimentary Deryugin and Tinro basins, which is characteristic of petroliferous basins.

AB - Potential field anomalies of the Sea of Okhotsk region are analyzed for compiling a map of the basement's tectonic structures. A 3D density model of the Earth's crust is constructed using seismogeological and experimental-petrophysical data, which made it possible to obtain a visual image of main structures of the region reflecting the observable geophysical anomalies. The obtained data allow a domain located in the central part of the Sea of Okhotsk beyond the limits of the exclusive economic zone of the Russian Federation to be considered as a natural continuation of the continental shelf since the latter is structurally similar to western Kamchatka. The deep structural boundaries rise beneath the large sedimentary Deryugin and Tinro basins, which is characteristic of petroliferous basins.

UR - http://www.scopus.com/inward/record.url?scp=84863091144&partnerID=8YFLogxK

U2 - 10.1134/S0001437012030095

DO - 10.1134/S0001437012030095

M3 - Article

AN - SCOPUS:84863091144

VL - 52

SP - 411

EP - 421

JO - Oceanology

JF - Oceanology

SN - 0001-4370

IS - 3

ER -

ID: 36844002