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Lomonosov ridge. / Piskarev, Alexey L.; Butsenko, Victor V.; Chernykh, Andrey A.; Ivanov, Mikhail V.; Kaminsky, Valery D.; Poselov, Victor A.; Savin, Vasily A.

Geologic Structures of the Arctic Basin. ed. / Alexey Piskarev; Victor Poselov; Valery Kaminsky. Springer Nature, 2018. p. 157-185.

Research output: Chapter in Book/Report/Conference proceeding › Chapter › peer-review

Harvard

Piskarev, AL, Butsenko, VV, Chernykh, AA, Ivanov, MV, Kaminsky, VD, Poselov, VA & Savin, VA 2018, Lomonosov ridge. in A Piskarev, V Poselov & V Kaminsky (eds), Geologic Structures of the Arctic Basin. Springer Nature, pp. 157-185. https://doi.org/10.1007/978-3-319-77742-9_4

APA

Piskarev, A. L., Butsenko, V. V., Chernykh, A. A., Ivanov, M. V., Kaminsky, V. D., Poselov, V. A., & Savin, V. A. (2018). Lomonosov ridge. In A. Piskarev, V. Poselov, & V. Kaminsky (Eds.), Geologic Structures of the Arctic Basin (pp. 157-185). Springer Nature. https://doi.org/10.1007/978-3-319-77742-9_4

Vancouver

Piskarev AL, Butsenko VV, Chernykh AA, Ivanov MV, Kaminsky VD, Poselov VA et al. Lomonosov ridge. In Piskarev A, Poselov V, Kaminsky V, editors, Geologic Structures of the Arctic Basin. Springer Nature. 2018. p. 157-185 https://doi.org/10.1007/978-3-319-77742-9_4

Author

Piskarev, Alexey L. ; Butsenko, Victor V. ; Chernykh, Andrey A. ; Ivanov, Mikhail V. ; Kaminsky, Valery D. ; Poselov, Victor A. ; Savin, Vasily A. / Lomonosov ridge. Geologic Structures of the Arctic Basin. editor / Alexey Piskarev ; Victor Poselov ; Valery Kaminsky. Springer Nature, 2018. pp. 157-185

BibTeX

@inbook{8f3fd8b450104aef910ce49655c8af54,
title = "Lomonosov ridge",
abstract = "The Lomonosov Ridge is situated between oceanic abyssal regions of the Eurasian Basin, on the one side, and the region of the Central Arctic Uplifts including the abyssal Makarov Basin - on the other. As its morphology and internal structure indicate, it consists of three distinct segments. The shallowest (= 400 m) Canada-Greenland segment is composed mostly by felsic and metamorphic rocks (basic igneous - at the part facing Alpha-Ridge). In the Near-Polar segment the ridge has double-crested top with the basin in-between. The structural trend here is at acute angle to the ridge axis and upper crust consists of basic crystalline rocks. The 12 km-thick upper crust of the 150 km-wide Siberian segment of the Lomonosov Ridge consists mainly of felsic and metamorphic rocks. The ridge's continental crystalline crust is 20-22 km thick, with upper and lower crusts thickness of about half of the above. Neogene-Pleistocene hemipelagic, Paleogene bathyal and possible Cretaceous deposits comprise the sedimentary cover.",
keywords = "Continental crust, Lomonosov Ridge, Morphology, Sedimentary cover",
author = "Piskarev, {Alexey L.} and Butsenko, {Victor V.} and Chernykh, {Andrey A.} and Ivanov, {Mikhail V.} and Kaminsky, {Valery D.} and Poselov, {Victor A.} and Savin, {Vasily A.}",
year = "2018",
month = jun,
day = "11",
doi = "10.1007/978-3-319-77742-9_4",
language = "English",
isbn = "9783319777412",
pages = "157--185",
editor = "Alexey Piskarev and Victor Poselov and Valery Kaminsky",
booktitle = "Geologic Structures of the Arctic Basin",
publisher = "Springer Nature",
address = "Germany",

}

RIS

TY - CHAP

T1 - Lomonosov ridge

AU - Piskarev, Alexey L.

AU - Butsenko, Victor V.

AU - Chernykh, Andrey A.

AU - Ivanov, Mikhail V.

AU - Kaminsky, Valery D.

AU - Poselov, Victor A.

AU - Savin, Vasily A.

PY - 2018/6/11

Y1 - 2018/6/11

N2 - The Lomonosov Ridge is situated between oceanic abyssal regions of the Eurasian Basin, on the one side, and the region of the Central Arctic Uplifts including the abyssal Makarov Basin - on the other. As its morphology and internal structure indicate, it consists of three distinct segments. The shallowest (= 400 m) Canada-Greenland segment is composed mostly by felsic and metamorphic rocks (basic igneous - at the part facing Alpha-Ridge). In the Near-Polar segment the ridge has double-crested top with the basin in-between. The structural trend here is at acute angle to the ridge axis and upper crust consists of basic crystalline rocks. The 12 km-thick upper crust of the 150 km-wide Siberian segment of the Lomonosov Ridge consists mainly of felsic and metamorphic rocks. The ridge's continental crystalline crust is 20-22 km thick, with upper and lower crusts thickness of about half of the above. Neogene-Pleistocene hemipelagic, Paleogene bathyal and possible Cretaceous deposits comprise the sedimentary cover.

AB - The Lomonosov Ridge is situated between oceanic abyssal regions of the Eurasian Basin, on the one side, and the region of the Central Arctic Uplifts including the abyssal Makarov Basin - on the other. As its morphology and internal structure indicate, it consists of three distinct segments. The shallowest (= 400 m) Canada-Greenland segment is composed mostly by felsic and metamorphic rocks (basic igneous - at the part facing Alpha-Ridge). In the Near-Polar segment the ridge has double-crested top with the basin in-between. The structural trend here is at acute angle to the ridge axis and upper crust consists of basic crystalline rocks. The 12 km-thick upper crust of the 150 km-wide Siberian segment of the Lomonosov Ridge consists mainly of felsic and metamorphic rocks. The ridge's continental crystalline crust is 20-22 km thick, with upper and lower crusts thickness of about half of the above. Neogene-Pleistocene hemipelagic, Paleogene bathyal and possible Cretaceous deposits comprise the sedimentary cover.

KW - Continental crust

KW - Lomonosov Ridge

KW - Morphology

KW - Sedimentary cover

UR - http://www.scopus.com/inward/record.url?scp=85053488873&partnerID=8YFLogxK

U2 - 10.1007/978-3-319-77742-9_4

DO - 10.1007/978-3-319-77742-9_4

M3 - Chapter

AN - SCOPUS:85053488873

SN - 9783319777412

SP - 157

EP - 185

BT - Geologic Structures of the Arctic Basin

A2 - Piskarev, Alexey

A2 - Poselov, Victor

A2 - Kaminsky, Valery

PB - Springer Nature

ER -

ID: 35884991