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Makarov Basin. / Piskarev, Alexey L.; Firsov, Yury G.; Poselov, Victor A.; Smirnov, Oleg E.

Geologic Structures of the Arctic Basin. Springer Nature, 2018. стр. 227-238.

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

Harvard

Piskarev, AL, Firsov, YG, Poselov, VA & Smirnov, OE 2018, Makarov Basin. в Geologic Structures of the Arctic Basin. Springer Nature, стр. 227-238. https://doi.org/10.1007/978-3-319-77742-9_6

APA

Piskarev, A. L., Firsov, Y. G., Poselov, V. A., & Smirnov, O. E. (2018). Makarov Basin. в Geologic Structures of the Arctic Basin (стр. 227-238). Springer Nature. https://doi.org/10.1007/978-3-319-77742-9_6

Vancouver

Piskarev AL, Firsov YG, Poselov VA, Smirnov OE. Makarov Basin. в Geologic Structures of the Arctic Basin. Springer Nature. 2018. стр. 227-238 https://doi.org/10.1007/978-3-319-77742-9_6

Author

Piskarev, Alexey L. ; Firsov, Yury G. ; Poselov, Victor A. ; Smirnov, Oleg E. / Makarov Basin. Geologic Structures of the Arctic Basin. Springer Nature, 2018. стр. 227-238

BibTeX

@inbook{43d7c8ecff864ff5b122b5526cd9b576,
title = "Makarov Basin",
abstract = "Makarov Basin - abyssal plain, 3800 m bsl on average (occasionally- over 4000 m, very close to the depth of the Nansen and Canada Basins), is mostly flat, disturbed only by 800 m-high linear ridge - abyssal continuation of the Marvin Spur. The potential fields anomalies illustrate the variety of structural plans of the Makarov Basin and surrounding regions. Gravity anomalies inside the Makarov Basin display symmetrical pattern relative to the linear positive anomaly parallel to 120°E, flanked by gravity lows on both side. The total thickness of the sedimentary cover varies from 2 to 4 km. The regional pre-Miocene unconformity RU at the base of the hemipelagic Miocene deposits is traceable through the whole Makarov Basin. The reduced Paleogene complex between the RU and post-Campanian unconformity pCU overlays the Upper Cretaceous and, possibly, older formations. Upper and lower crusts are estimated to be 3-6 km and 3-4 km, accordingly. Total crust thickness is 10-12 km.",
keywords = "Earth's crust, Gravity, Magnetic anomalies, Makarov basin, Sedimentary cover",
author = "Piskarev, {Alexey L.} and Firsov, {Yury G.} and Poselov, {Victor A.} and Smirnov, {Oleg E.}",
year = "2018",
month = jun,
day = "11",
doi = "10.1007/978-3-319-77742-9_6",
language = "English",
isbn = "9783319777412",
pages = "227--238",
booktitle = "Geologic Structures of the Arctic Basin",
publisher = "Springer Nature",
address = "Germany",

}

RIS

TY - CHAP

T1 - Makarov Basin

AU - Piskarev, Alexey L.

AU - Firsov, Yury G.

AU - Poselov, Victor A.

AU - Smirnov, Oleg E.

PY - 2018/6/11

Y1 - 2018/6/11

N2 - Makarov Basin - abyssal plain, 3800 m bsl on average (occasionally- over 4000 m, very close to the depth of the Nansen and Canada Basins), is mostly flat, disturbed only by 800 m-high linear ridge - abyssal continuation of the Marvin Spur. The potential fields anomalies illustrate the variety of structural plans of the Makarov Basin and surrounding regions. Gravity anomalies inside the Makarov Basin display symmetrical pattern relative to the linear positive anomaly parallel to 120°E, flanked by gravity lows on both side. The total thickness of the sedimentary cover varies from 2 to 4 km. The regional pre-Miocene unconformity RU at the base of the hemipelagic Miocene deposits is traceable through the whole Makarov Basin. The reduced Paleogene complex between the RU and post-Campanian unconformity pCU overlays the Upper Cretaceous and, possibly, older formations. Upper and lower crusts are estimated to be 3-6 km and 3-4 km, accordingly. Total crust thickness is 10-12 km.

AB - Makarov Basin - abyssal plain, 3800 m bsl on average (occasionally- over 4000 m, very close to the depth of the Nansen and Canada Basins), is mostly flat, disturbed only by 800 m-high linear ridge - abyssal continuation of the Marvin Spur. The potential fields anomalies illustrate the variety of structural plans of the Makarov Basin and surrounding regions. Gravity anomalies inside the Makarov Basin display symmetrical pattern relative to the linear positive anomaly parallel to 120°E, flanked by gravity lows on both side. The total thickness of the sedimentary cover varies from 2 to 4 km. The regional pre-Miocene unconformity RU at the base of the hemipelagic Miocene deposits is traceable through the whole Makarov Basin. The reduced Paleogene complex between the RU and post-Campanian unconformity pCU overlays the Upper Cretaceous and, possibly, older formations. Upper and lower crusts are estimated to be 3-6 km and 3-4 km, accordingly. Total crust thickness is 10-12 km.

KW - Earth's crust

KW - Gravity

KW - Magnetic anomalies

KW - Makarov basin

KW - Sedimentary cover

UR - http://www.scopus.com/inward/record.url?scp=85053505717&partnerID=8YFLogxK

U2 - 10.1007/978-3-319-77742-9_6

DO - 10.1007/978-3-319-77742-9_6

M3 - Chapter

AN - SCOPUS:85053505717

SN - 9783319777412

SP - 227

EP - 238

BT - Geologic Structures of the Arctic Basin

PB - Springer Nature

ER -

ID: 36842555