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Podvodnikov Basin. / Smirnov, Oleg E.; Butsenko, Victor V.; Firsov, Yury G.; Glebovsky, Vladimir Yu; Gusev, Evgeny A.; Kaminsky, Valery D.; Kazanin, Gennady S.; Piskarev, Alexey L.; Poselov, Victor A.

Geologic Structures of the Arctic Basin. Springer Nature, 2018. стр. 187-225.

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

Harvard

Smirnov, OE, Butsenko, VV, Firsov, YG, Glebovsky, VY, Gusev, EA, Kaminsky, VD, Kazanin, GS, Piskarev, AL & Poselov, VA 2018, Podvodnikov Basin. в Geologic Structures of the Arctic Basin. Springer Nature, стр. 187-225. https://doi.org/10.1007/978-3-319-77742-9_5

APA

Smirnov, O. E., Butsenko, V. V., Firsov, Y. G., Glebovsky, V. Y., Gusev, E. A., Kaminsky, V. D., Kazanin, G. S., Piskarev, A. L., & Poselov, V. A. (2018). Podvodnikov Basin. в Geologic Structures of the Arctic Basin (стр. 187-225). Springer Nature. https://doi.org/10.1007/978-3-319-77742-9_5

Vancouver

Smirnov OE, Butsenko VV, Firsov YG, Glebovsky VY, Gusev EA, Kaminsky VD и пр. Podvodnikov Basin. в Geologic Structures of the Arctic Basin. Springer Nature. 2018. стр. 187-225 https://doi.org/10.1007/978-3-319-77742-9_5

Author

Smirnov, Oleg E. ; Butsenko, Victor V. ; Firsov, Yury G. ; Glebovsky, Vladimir Yu ; Gusev, Evgeny A. ; Kaminsky, Valery D. ; Kazanin, Gennady S. ; Piskarev, Alexey L. ; Poselov, Victor A. / Podvodnikov Basin. Geologic Structures of the Arctic Basin. Springer Nature, 2018. стр. 187-225

BibTeX

@inbook{d54093f2868841a3929e62e383fb5240,
title = "Podvodnikov Basin",
abstract = "The vast bathymetric depression of the Podvodnikov Basin lies between the Lomonosov Ridge and Mendeleev - Alpha Ridges, bounded by the East-Siberian Sea shelf from the south and by the Makarov Basin - from the north. Sea depth in the Podvodnikov Basin varies from 800 m to 2700 m in the same direction. The Podvodnikov Basin has a benched structure and is considered to be a part of the terraced continental slope. The seismic data divide the southern terrace of the Podvodnikov Basin into western and eastern parts, separated by the prominent Geofizikov Spur and its southern continuation as a deeper structure of the acoustic basement. Total thickness of the sedimentary cover here reaches 8 km. The sedimentary cover of the Podvodnikov Basin is subdivided into six seismic-stratigraphic complexes, dated from late Permian to Holocene by correlation with ACEX well on the Lomonosov Ridge and exploration wells on the Alaska shelf. Integrated geophysical data interpretation and modeling classify the Basin's crust as stretched continental, with thickness of the crystalline crust from 10 to 23 km.",
keywords = "Bathymetric depression, Extended continental crust, Extension structure, Geofizikov Spur, Podvodnikov Basin, Sedimentary basin",
author = "Smirnov, {Oleg E.} and Butsenko, {Victor V.} and Firsov, {Yury G.} and Glebovsky, {Vladimir Yu} and Gusev, {Evgeny A.} and Kaminsky, {Valery D.} and Kazanin, {Gennady S.} and Piskarev, {Alexey L.} and Poselov, {Victor A.}",
year = "2018",
month = jun,
day = "11",
doi = "10.1007/978-3-319-77742-9_5",
language = "English",
isbn = "9783319777412",
pages = "187--225",
booktitle = "Geologic Structures of the Arctic Basin",
publisher = "Springer Nature",
address = "Germany",

}

RIS

TY - CHAP

T1 - Podvodnikov Basin

AU - Smirnov, Oleg E.

AU - Butsenko, Victor V.

AU - Firsov, Yury G.

AU - Glebovsky, Vladimir Yu

AU - Gusev, Evgeny A.

AU - Kaminsky, Valery D.

AU - Kazanin, Gennady S.

AU - Piskarev, Alexey L.

AU - Poselov, Victor A.

PY - 2018/6/11

Y1 - 2018/6/11

N2 - The vast bathymetric depression of the Podvodnikov Basin lies between the Lomonosov Ridge and Mendeleev - Alpha Ridges, bounded by the East-Siberian Sea shelf from the south and by the Makarov Basin - from the north. Sea depth in the Podvodnikov Basin varies from 800 m to 2700 m in the same direction. The Podvodnikov Basin has a benched structure and is considered to be a part of the terraced continental slope. The seismic data divide the southern terrace of the Podvodnikov Basin into western and eastern parts, separated by the prominent Geofizikov Spur and its southern continuation as a deeper structure of the acoustic basement. Total thickness of the sedimentary cover here reaches 8 km. The sedimentary cover of the Podvodnikov Basin is subdivided into six seismic-stratigraphic complexes, dated from late Permian to Holocene by correlation with ACEX well on the Lomonosov Ridge and exploration wells on the Alaska shelf. Integrated geophysical data interpretation and modeling classify the Basin's crust as stretched continental, with thickness of the crystalline crust from 10 to 23 km.

AB - The vast bathymetric depression of the Podvodnikov Basin lies between the Lomonosov Ridge and Mendeleev - Alpha Ridges, bounded by the East-Siberian Sea shelf from the south and by the Makarov Basin - from the north. Sea depth in the Podvodnikov Basin varies from 800 m to 2700 m in the same direction. The Podvodnikov Basin has a benched structure and is considered to be a part of the terraced continental slope. The seismic data divide the southern terrace of the Podvodnikov Basin into western and eastern parts, separated by the prominent Geofizikov Spur and its southern continuation as a deeper structure of the acoustic basement. Total thickness of the sedimentary cover here reaches 8 km. The sedimentary cover of the Podvodnikov Basin is subdivided into six seismic-stratigraphic complexes, dated from late Permian to Holocene by correlation with ACEX well on the Lomonosov Ridge and exploration wells on the Alaska shelf. Integrated geophysical data interpretation and modeling classify the Basin's crust as stretched continental, with thickness of the crystalline crust from 10 to 23 km.

KW - Bathymetric depression

KW - Extended continental crust

KW - Extension structure

KW - Geofizikov Spur

KW - Podvodnikov Basin

KW - Sedimentary basin

UR - http://www.scopus.com/inward/record.url?scp=85053513331&partnerID=8YFLogxK

U2 - 10.1007/978-3-319-77742-9_5

DO - 10.1007/978-3-319-77742-9_5

M3 - Chapter

AN - SCOPUS:85053513331

SN - 9783319777412

SP - 187

EP - 225

BT - Geologic Structures of the Arctic Basin

PB - Springer Nature

ER -

ID: 36842841