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Structure of the Earth’s Crust of the Continental Margin of the Laptev Sea and the Adjacent Part of the Eurasian Basin. / Piskarev, A. L.; Kaminsky, V. D.; Poselov, V. A.; Bezumov, D. V.; Zholondz, S. M.; Kireev, A. A.; Ovanesian, G. I.; Savin, V. A.; Smirnov, O. E.

в: Doklady Earth Sciences, Том 511, № 2, 18.07.2023, стр. 692–697.

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

Harvard

Piskarev, AL, Kaminsky, VD, Poselov, VA, Bezumov, DV, Zholondz, SM, Kireev, AA, Ovanesian, GI, Savin, VA & Smirnov, OE 2023, 'Structure of the Earth’s Crust of the Continental Margin of the Laptev Sea and the Adjacent Part of the Eurasian Basin', Doklady Earth Sciences, Том. 511, № 2, стр. 692–697. https://doi.org/10.1134/s1028334x23600883

APA

Piskarev, A. L., Kaminsky, V. D., Poselov, V. A., Bezumov, D. V., Zholondz, S. M., Kireev, A. A., Ovanesian, G. I., Savin, V. A., & Smirnov, O. E. (2023). Structure of the Earth’s Crust of the Continental Margin of the Laptev Sea and the Adjacent Part of the Eurasian Basin. Doklady Earth Sciences, 511(2), 692–697. https://doi.org/10.1134/s1028334x23600883

Vancouver

Piskarev AL, Kaminsky VD, Poselov VA, Bezumov DV, Zholondz SM, Kireev AA и пр. Structure of the Earth’s Crust of the Continental Margin of the Laptev Sea and the Adjacent Part of the Eurasian Basin. Doklady Earth Sciences. 2023 Июль 18;511(2):692–697. https://doi.org/10.1134/s1028334x23600883

Author

Piskarev, A. L. ; Kaminsky, V. D. ; Poselov, V. A. ; Bezumov, D. V. ; Zholondz, S. M. ; Kireev, A. A. ; Ovanesian, G. I. ; Savin, V. A. ; Smirnov, O. E. / Structure of the Earth’s Crust of the Continental Margin of the Laptev Sea and the Adjacent Part of the Eurasian Basin. в: Doklady Earth Sciences. 2023 ; Том 511, № 2. стр. 692–697.

BibTeX

@article{ce858326b31841c9af2a4f08f4b3f9f7,
title = "Structure of the Earth{\textquoteright}s Crust of the Continental Margin of the Laptev Sea and the Adjacent Part of the Eurasian Basin",
abstract = "Abstract: A 3D model of the Earth{\textquoteright}s crust for the continental margin of the Laptev Sea and the adjacent part of the Eurasian Basin was developed using the latest seismic and gravity data. The thickness of the consolidated part of the Earth{\textquoteright}s crust in the study area is estimated at 7–11 km, which corresponds to a highly extended continental or oceanic crust. The formation of the basement and sedimentation in this area most likely began in the Late Jurassic. The southeastern part of the Eurasian Basin is separated from the rest of the basin by a dextral shear zone, the displacement along which during the Paleogene was more than 100 km.",
keywords = "Earth{\textquoteright}s crust, Eurasian Basin, Laptev Sea, geophysical modeling, tectonics",
author = "Piskarev, {A. L.} and Kaminsky, {V. D.} and Poselov, {V. A.} and Bezumov, {D. V.} and Zholondz, {S. M.} and Kireev, {A. A.} and Ovanesian, {G. I.} and Savin, {V. A.} and Smirnov, {O. E.}",
year = "2023",
month = jul,
day = "18",
doi = "10.1134/s1028334x23600883",
language = "English",
volume = "511",
pages = "692–697",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

TY - JOUR

T1 - Structure of the Earth’s Crust of the Continental Margin of the Laptev Sea and the Adjacent Part of the Eurasian Basin

AU - Piskarev, A. L.

AU - Kaminsky, V. D.

AU - Poselov, V. A.

AU - Bezumov, D. V.

AU - Zholondz, S. M.

AU - Kireev, A. A.

AU - Ovanesian, G. I.

AU - Savin, V. A.

AU - Smirnov, O. E.

PY - 2023/7/18

Y1 - 2023/7/18

N2 - Abstract: A 3D model of the Earth’s crust for the continental margin of the Laptev Sea and the adjacent part of the Eurasian Basin was developed using the latest seismic and gravity data. The thickness of the consolidated part of the Earth’s crust in the study area is estimated at 7–11 km, which corresponds to a highly extended continental or oceanic crust. The formation of the basement and sedimentation in this area most likely began in the Late Jurassic. The southeastern part of the Eurasian Basin is separated from the rest of the basin by a dextral shear zone, the displacement along which during the Paleogene was more than 100 km.

AB - Abstract: A 3D model of the Earth’s crust for the continental margin of the Laptev Sea and the adjacent part of the Eurasian Basin was developed using the latest seismic and gravity data. The thickness of the consolidated part of the Earth’s crust in the study area is estimated at 7–11 km, which corresponds to a highly extended continental or oceanic crust. The formation of the basement and sedimentation in this area most likely began in the Late Jurassic. The southeastern part of the Eurasian Basin is separated from the rest of the basin by a dextral shear zone, the displacement along which during the Paleogene was more than 100 km.

KW - Earth’s crust

KW - Eurasian Basin

KW - Laptev Sea

KW - geophysical modeling

KW - tectonics

UR - https://www.mendeley.com/catalogue/613c3d2d-2da0-314f-85ca-aceb114ba1f4/

U2 - 10.1134/s1028334x23600883

DO - 10.1134/s1028334x23600883

M3 - Article

VL - 511

SP - 692

EP - 697

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 110933646