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Eurasian Basin. / Savin, Vasily A.; Avetisov, Georgy P.; Artem'eva, Daria E.; Bezumov, Dmitry V.; Chernykh, Andrey A.; Glebovsky, Vladimir Yu; Kazanin, Gennady S.; Piskarev, Alexey L.

Geologic Structures of the Arctic Basin. Springer Nature, 2018. p. 105-155 (Geologic Structures of the Arctic Basin).

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

Harvard

Savin, VA, Avetisov, GP, Artem'eva, DE, Bezumov, DV, Chernykh, AA, Glebovsky, VY, Kazanin, GS & Piskarev, AL 2018, Eurasian Basin. in Geologic Structures of the Arctic Basin. Geologic Structures of the Arctic Basin, Springer Nature, pp. 105-155. https://doi.org/10.1007/978-3-319-77742-9_3

APA

Savin, V. A., Avetisov, G. P., Artem'eva, D. E., Bezumov, D. V., Chernykh, A. A., Glebovsky, V. Y., Kazanin, G. S., & Piskarev, A. L. (2018). Eurasian Basin. In Geologic Structures of the Arctic Basin (pp. 105-155). (Geologic Structures of the Arctic Basin). Springer Nature. https://doi.org/10.1007/978-3-319-77742-9_3

Vancouver

Savin VA, Avetisov GP, Artem'eva DE, Bezumov DV, Chernykh AA, Glebovsky VY et al. Eurasian Basin. In Geologic Structures of the Arctic Basin. Springer Nature. 2018. p. 105-155. (Geologic Structures of the Arctic Basin). https://doi.org/10.1007/978-3-319-77742-9_3

Author

Savin, Vasily A. ; Avetisov, Georgy P. ; Artem'eva, Daria E. ; Bezumov, Dmitry V. ; Chernykh, Andrey A. ; Glebovsky, Vladimir Yu ; Kazanin, Gennady S. ; Piskarev, Alexey L. / Eurasian Basin. Geologic Structures of the Arctic Basin. Springer Nature, 2018. pp. 105-155 (Geologic Structures of the Arctic Basin).

BibTeX

@inbook{aef1c1ff83be47ef8d982aafb0869d89,
title = "Eurasian Basin",
abstract = "The Eurasian Basin, ~2000 km long and ~900 km wide, consists of abyssal plains of Nansen and Amundsen Basins separated by mid-oceanic Gakkel Ridge. The magnetic field of the Eurasian Basin consists mostly of linear magnetic anomalies (LMA). According to classic hypothesis, anomalies of Cenozoic sequence, from LMA 24 (chron 24, ~53 Ma) to present, were identified and dated. Steady decline of spreading velocity from 22-27 mm/yr. to 5-9 mm/yr. was established for 53-20 Ma interval; later it grew slightly to 7-12 mm/yr. At the same time pronounced asymmetry of geological, morphological and bathymetry features of the abyssal depressions, as well as demonstrated by seismic data asymmetry of distribution and thickness variations of sedimentary formations inside them, lead us to conclusion that the considerable part of the Eurasian Basin was probably formed in pre-Cenozoic time.",
keywords = "Amundsen Basin, Cenozoic oceanic basement, Eurasian Basin, Gakkel Ridge, Nansen Basin, Pre-Cenozoic oceanic basement, Spreading velocity",
author = "Savin, {Vasily A.} and Avetisov, {Georgy P.} and Artem'eva, {Daria E.} and Bezumov, {Dmitry V.} and Chernykh, {Andrey A.} and Glebovsky, {Vladimir Yu} and Kazanin, {Gennady S.} and Piskarev, {Alexey L.}",
year = "2018",
month = jun,
day = "11",
doi = "10.1007/978-3-319-77742-9_3",
language = "English",
isbn = "9783319777412",
series = "Geologic Structures of the Arctic Basin",
publisher = "Springer Nature",
pages = "105--155",
booktitle = "Geologic Structures of the Arctic Basin",
address = "Germany",

}

RIS

TY - CHAP

T1 - Eurasian Basin

AU - Savin, Vasily A.

AU - Avetisov, Georgy P.

AU - Artem'eva, Daria E.

AU - Bezumov, Dmitry V.

AU - Chernykh, Andrey A.

AU - Glebovsky, Vladimir Yu

AU - Kazanin, Gennady S.

AU - Piskarev, Alexey L.

PY - 2018/6/11

Y1 - 2018/6/11

N2 - The Eurasian Basin, ~2000 km long and ~900 km wide, consists of abyssal plains of Nansen and Amundsen Basins separated by mid-oceanic Gakkel Ridge. The magnetic field of the Eurasian Basin consists mostly of linear magnetic anomalies (LMA). According to classic hypothesis, anomalies of Cenozoic sequence, from LMA 24 (chron 24, ~53 Ma) to present, were identified and dated. Steady decline of spreading velocity from 22-27 mm/yr. to 5-9 mm/yr. was established for 53-20 Ma interval; later it grew slightly to 7-12 mm/yr. At the same time pronounced asymmetry of geological, morphological and bathymetry features of the abyssal depressions, as well as demonstrated by seismic data asymmetry of distribution and thickness variations of sedimentary formations inside them, lead us to conclusion that the considerable part of the Eurasian Basin was probably formed in pre-Cenozoic time.

AB - The Eurasian Basin, ~2000 km long and ~900 km wide, consists of abyssal plains of Nansen and Amundsen Basins separated by mid-oceanic Gakkel Ridge. The magnetic field of the Eurasian Basin consists mostly of linear magnetic anomalies (LMA). According to classic hypothesis, anomalies of Cenozoic sequence, from LMA 24 (chron 24, ~53 Ma) to present, were identified and dated. Steady decline of spreading velocity from 22-27 mm/yr. to 5-9 mm/yr. was established for 53-20 Ma interval; later it grew slightly to 7-12 mm/yr. At the same time pronounced asymmetry of geological, morphological and bathymetry features of the abyssal depressions, as well as demonstrated by seismic data asymmetry of distribution and thickness variations of sedimentary formations inside them, lead us to conclusion that the considerable part of the Eurasian Basin was probably formed in pre-Cenozoic time.

KW - Amundsen Basin

KW - Cenozoic oceanic basement

KW - Eurasian Basin

KW - Gakkel Ridge

KW - Nansen Basin

KW - Pre-Cenozoic oceanic basement

KW - Spreading velocity

UR - http://www.scopus.com/inward/record.url?scp=85053517836&partnerID=8YFLogxK

U2 - 10.1007/978-3-319-77742-9_3

DO - 10.1007/978-3-319-77742-9_3

M3 - Chapter

AN - SCOPUS:85053517836

SN - 9783319777412

T3 - Geologic Structures of the Arctic Basin

SP - 105

EP - 155

BT - Geologic Structures of the Arctic Basin

PB - Springer Nature

ER -

ID: 35882212