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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. ред. / Alexey Piskarev; Victor Poselov; Valery Kaminsky. Springer Nature, 2018. стр. 157-185.

Результаты исследований: Публикации в книгах, отчётах, сборниках, трудах конференций › глава/раздел › научная › Рецензирование

Harvard

Piskarev, AL, Butsenko, VV, Chernykh, AA, Ivanov, MV, Kaminsky, VD, Poselov, VA & Savin, VA 2018, Lomonosov ridge. в A Piskarev, V Poselov & V Kaminsky (ред.), Geologic Structures of the Arctic Basin. Springer Nature, стр. 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. в A. Piskarev, V. Poselov, & V. Kaminsky (Ред.), Geologic Structures of the Arctic Basin (стр. 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 и пр. Lomonosov ridge. в Piskarev A, Poselov V, Kaminsky V, Редакторы, Geologic Structures of the Arctic Basin. Springer Nature. 2018. стр. 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. Редактор / Alexey Piskarev ; Victor Poselov ; Valery Kaminsky. Springer Nature, 2018. стр. 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

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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