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Mendeleev and alpha ridges. / Butsenko, Victor V.; Firsov, Yury G.; Gusev, Evgeny A.; Kaminsky, Valery D.; Kashubin, Sergey P.; Piskarev, Alexey L.; Poselov, Victor A.

Geologic Structures of the Arctic Basin. Springer Nature, 2018. p. 239-268.

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

Harvard

Butsenko, VV, Firsov, YG, Gusev, EA, Kaminsky, VD, Kashubin, SP, Piskarev, AL & Poselov, VA 2018, Mendeleev and alpha ridges. in Geologic Structures of the Arctic Basin. Springer Nature, pp. 239-268. https://doi.org/10.1007/978-3-319-77742-9_7

APA

Butsenko, V. V., Firsov, Y. G., Gusev, E. A., Kaminsky, V. D., Kashubin, S. P., Piskarev, A. L., & Poselov, V. A. (2018). Mendeleev and alpha ridges. In Geologic Structures of the Arctic Basin (pp. 239-268). Springer Nature. https://doi.org/10.1007/978-3-319-77742-9_7

Vancouver

Butsenko VV, Firsov YG, Gusev EA, Kaminsky VD, Kashubin SP, Piskarev AL et al. Mendeleev and alpha ridges. In Geologic Structures of the Arctic Basin. Springer Nature. 2018. p. 239-268 https://doi.org/10.1007/978-3-319-77742-9_7

Author

Butsenko, Victor V. ; Firsov, Yury G. ; Gusev, Evgeny A. ; Kaminsky, Valery D. ; Kashubin, Sergey P. ; Piskarev, Alexey L. ; Poselov, Victor A. / Mendeleev and alpha ridges. Geologic Structures of the Arctic Basin. Springer Nature, 2018. pp. 239-268

BibTeX

@inbook{fb347af1f6404a12973c2df08aed3e51,
title = "Mendeleev and alpha ridges",
abstract = "The Mendeleev Ridge was formed on the continental crust with total thickness 27-32 km of which the upper crust takes 4-7 km. Continuous chain of progressively seaward deepening bathymetric terraces demonstrate the morphological connection of the Mendeleev Ridge with shallow water regions of the Siberian-Chukchi continental margin. Seismic data reveal that the structure and stratigraphy of the Mendeleev Ridge are affected by intensive normal faulting of acoustic basement creating complex system of grabens and half-grabens. It depicts the Mendeleev Ridge as an extensional structure of Cretaceous age illustrating tectonic evolution of the Central Arctic region. The Miocene-Pleistocene complex, with continuous undisturbed layers of hemipelagic sediments and regional erosional unconformity at its base, drapes the entire Mendeleev Ridge and marks the completion of contemporary morphological modern system of the Mendeleev-Alpha Ridge System.",
keywords = "Alpha Ridge, Continental crust, Extensional structure, Mendeleev Ridge, Normal faults, Sedimentary cover",
author = "Butsenko, {Victor V.} and Firsov, {Yury G.} and Gusev, {Evgeny A.} and Kaminsky, {Valery D.} and Kashubin, {Sergey P.} and Piskarev, {Alexey L.} and Poselov, {Victor A.}",
year = "2018",
month = jun,
day = "11",
doi = "10.1007/978-3-319-77742-9_7",
language = "English",
isbn = "9783319777412",
pages = "239--268",
booktitle = "Geologic Structures of the Arctic Basin",
publisher = "Springer Nature",
address = "Germany",

}

RIS

TY - CHAP

T1 - Mendeleev and alpha ridges

AU - Butsenko, Victor V.

AU - Firsov, Yury G.

AU - Gusev, Evgeny A.

AU - Kaminsky, Valery D.

AU - Kashubin, Sergey P.

AU - Piskarev, Alexey L.

AU - Poselov, Victor A.

PY - 2018/6/11

Y1 - 2018/6/11

N2 - The Mendeleev Ridge was formed on the continental crust with total thickness 27-32 km of which the upper crust takes 4-7 km. Continuous chain of progressively seaward deepening bathymetric terraces demonstrate the morphological connection of the Mendeleev Ridge with shallow water regions of the Siberian-Chukchi continental margin. Seismic data reveal that the structure and stratigraphy of the Mendeleev Ridge are affected by intensive normal faulting of acoustic basement creating complex system of grabens and half-grabens. It depicts the Mendeleev Ridge as an extensional structure of Cretaceous age illustrating tectonic evolution of the Central Arctic region. The Miocene-Pleistocene complex, with continuous undisturbed layers of hemipelagic sediments and regional erosional unconformity at its base, drapes the entire Mendeleev Ridge and marks the completion of contemporary morphological modern system of the Mendeleev-Alpha Ridge System.

AB - The Mendeleev Ridge was formed on the continental crust with total thickness 27-32 km of which the upper crust takes 4-7 km. Continuous chain of progressively seaward deepening bathymetric terraces demonstrate the morphological connection of the Mendeleev Ridge with shallow water regions of the Siberian-Chukchi continental margin. Seismic data reveal that the structure and stratigraphy of the Mendeleev Ridge are affected by intensive normal faulting of acoustic basement creating complex system of grabens and half-grabens. It depicts the Mendeleev Ridge as an extensional structure of Cretaceous age illustrating tectonic evolution of the Central Arctic region. The Miocene-Pleistocene complex, with continuous undisturbed layers of hemipelagic sediments and regional erosional unconformity at its base, drapes the entire Mendeleev Ridge and marks the completion of contemporary morphological modern system of the Mendeleev-Alpha Ridge System.

KW - Alpha Ridge

KW - Continental crust

KW - Extensional structure

KW - Mendeleev Ridge

KW - Normal faults

KW - Sedimentary cover

UR - http://www.scopus.com/inward/record.url?scp=85053496159&partnerID=8YFLogxK

U2 - 10.1007/978-3-319-77742-9_7

DO - 10.1007/978-3-319-77742-9_7

M3 - Chapter

AN - SCOPUS:85053496159

SN - 9783319777412

SP - 239

EP - 268

BT - Geologic Structures of the Arctic Basin

PB - Springer Nature

ER -

ID: 36842742