Deep structure of crust and the upper mantle of the Mendeleev Rise on the Arktic­-2012 DSS profile

Research output: Contribution to journal › Journal article › Research › peer-review

Standard

Deep structure of crust and the upper mantle of the Mendeleev Rise on the Arktic­-2012 DSS profile. / Kashubin, Sergey; Petrov, Oleg; Artemieva, Irina; Morozov, Andrey; Vyatkina, D.V.; Golysheva, Yu.S.; Kashubina, Tatiana; Milstein, E.D.; Erinchek, Yuri; Sakulina , T.S.; Krupnova, N.A.

In: Regional Geology and Metallogeny, Vol. 2016, No. 65, 01.02.2016, p. 16–36.

Research output: Contribution to journal › Journal article › Research › peer-review

Harvard

Kashubin, S, Petrov, O, Artemieva, I, Morozov, A, Vyatkina, DV, Golysheva, YS, Kashubina, T, Milstein, ED, Erinchek, Y, Sakulina , TS & Krupnova, NA 2016, 'Deep structure of crust and the upper mantle of the Mendeleev Rise on the Arktic­-2012 DSS profile', Regional Geology and Metallogeny, vol. 2016, no. 65, pp. 16–36.

APA

Kashubin, S., Petrov, O., Artemieva, I., Morozov, A., Vyatkina, D. V., Golysheva, Y. S., Kashubina, T., Milstein, E. D., Erinchek, Y., Sakulina , T. S., & Krupnova, N. A. (2016). Deep structure of crust and the upper mantle of the Mendeleev Rise on the Arktic­-2012 DSS profile. Regional Geology and Metallogeny, 2016(65), 16–36.

Vancouver

Kashubin S, Petrov O, Artemieva I, Morozov A, Vyatkina DV, Golysheva YS et al. Deep structure of crust and the upper mantle of the Mendeleev Rise on the Arktic­-2012 DSS profile. Regional Geology and Metallogeny. 2016 Feb 1;2016(65):16–36.

Author

Kashubin, Sergey ; Petrov, Oleg ; Artemieva, Irina ; Morozov, Andrey ; Vyatkina, D.V. ; Golysheva, Yu.S. ; Kashubina, Tatiana ; Milstein, E.D. ; Erinchek, Yuri ; Sakulina , T.S. ; Krupnova, N.A. / Deep structure of crust and the upper mantle of the Mendeleev Rise on the Arktic­-2012 DSS profile. In: Regional Geology and Metallogeny. 2016 ; Vol. 2016, No. 65. pp. 16–36.

Bibtex

@article{be4cd05fdd204455b6fc5fcf70460ddd,
title = "Deep structure of crust and the upper mantle of the Mendeleev Rise on the Arktic­-2012 DSS profile",
abstract = "During high­latitude combined geological and geophysical expedition “Arctic­-2012”, deep seismic sounding (DSS) with ocean bottom seismometers were carried out in the Arctic Ocean along the line 740 km long, crossing the Mendeleev Rise at about 77° N. Crustal and upper mantle Vp­velocity and Vp/Vs­ratio models were constructed. Crustal section comprises: sedimentary cover, intermediate (metasedimentary) complex, upper crystalline crust, lower crystalline crust, upper mantle. Crustal thickness within the Mendeleev Rise is about 32 km; almost 20 km falls on the lower crust. In general, velocity parameters and crustal thickness on the Mendeleev Rise are typical of continental crust. Increased thickness of the lower crust may be related to magmatic underplating, which in turn led to intraplate mafic volcanism and HALIP formation in this part of the Arctic. ",
author = "Sergey Kashubin and Oleg Petrov and Irina Artemieva and Andrey Morozov and D.V. Vyatkina and Yu.S. Golysheva and Tatiana Kashubina and E.D. Milstein and Yuri Erinchek and T.S. Sakulina and N.A. Krupnova",
year = "2016",
month = feb,
day = "1",
language = "Russisk",
volume = "2016",
pages = "16–36",
journal = "Regional Geology and Metallogeny",
issn = "0869-7892",
number = "65",

}

RIS

TY - JOUR

T1 - Deep structure of crust and the upper mantle of the Mendeleev Rise on the Arktic­-2012 DSS profile

AU - Kashubin, Sergey

AU - Petrov, Oleg

AU - Artemieva, Irina

AU - Morozov, Andrey

AU - Vyatkina, D.V.

AU - Golysheva, Yu.S.

AU - Kashubina, Tatiana

AU - Milstein, E.D.

AU - Erinchek, Yuri

AU - Sakulina , T.S.

AU - Krupnova, N.A.

PY - 2016/2/1

Y1 - 2016/2/1

N2 - During high­latitude combined geological and geophysical expedition “Arctic­-2012”, deep seismic sounding (DSS) with ocean bottom seismometers were carried out in the Arctic Ocean along the line 740 km long, crossing the Mendeleev Rise at about 77° N. Crustal and upper mantle Vp­velocity and Vp/Vs­ratio models were constructed. Crustal section comprises: sedimentary cover, intermediate (metasedimentary) complex, upper crystalline crust, lower crystalline crust, upper mantle. Crustal thickness within the Mendeleev Rise is about 32 km; almost 20 km falls on the lower crust. In general, velocity parameters and crustal thickness on the Mendeleev Rise are typical of continental crust. Increased thickness of the lower crust may be related to magmatic underplating, which in turn led to intraplate mafic volcanism and HALIP formation in this part of the Arctic.

AB - During high­latitude combined geological and geophysical expedition “Arctic­-2012”, deep seismic sounding (DSS) with ocean bottom seismometers were carried out in the Arctic Ocean along the line 740 km long, crossing the Mendeleev Rise at about 77° N. Crustal and upper mantle Vp­velocity and Vp/Vs­ratio models were constructed. Crustal section comprises: sedimentary cover, intermediate (metasedimentary) complex, upper crystalline crust, lower crystalline crust, upper mantle. Crustal thickness within the Mendeleev Rise is about 32 km; almost 20 km falls on the lower crust. In general, velocity parameters and crustal thickness on the Mendeleev Rise are typical of continental crust. Increased thickness of the lower crust may be related to magmatic underplating, which in turn led to intraplate mafic volcanism and HALIP formation in this part of the Arctic.

UR - http://www.vsegei.ru/en/rgm/content/2016/65/index.php

M3 - Tidsskriftartikel

VL - 2016

SP - 16

EP - 36

JO - Regional Geology and Metallogeny

JF - Regional Geology and Metallogeny

SN - 0869-7892

IS - 65

ER -

ID: 160428770