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Westward progradation of Meso-Cenozoic tectonic deformations in the Laptev and East Siberian Seas region. / Piskarev, A.; Kos'ko, M.

80th EAGE Conference and Exhibition 2018: Opportunities Presented by the Energy Transition. European Association of Geoscientists and Engineers, 2018. (80th EAGE Conference and Exhibition 2018: Opportunities Presented by the Energy Transition).

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

Harvard

Piskarev, A & Kos'ko, M 2018, Westward progradation of Meso-Cenozoic tectonic deformations in the Laptev and East Siberian Seas region. in 80th EAGE Conference and Exhibition 2018: Opportunities Presented by the Energy Transition. 80th EAGE Conference and Exhibition 2018: Opportunities Presented by the Energy Transition, European Association of Geoscientists and Engineers, 80th EAGE Conference and Exhibition 2018: Opportunities Presented by the Energy Transition, Copenhagen, Denmark, 11/06/18.

APA

Piskarev, A., & Kos'ko, M. (2018). Westward progradation of Meso-Cenozoic tectonic deformations in the Laptev and East Siberian Seas region. In 80th EAGE Conference and Exhibition 2018: Opportunities Presented by the Energy Transition (80th EAGE Conference and Exhibition 2018: Opportunities Presented by the Energy Transition). European Association of Geoscientists and Engineers.

Vancouver

Piskarev A, Kos'ko M. Westward progradation of Meso-Cenozoic tectonic deformations in the Laptev and East Siberian Seas region. In 80th EAGE Conference and Exhibition 2018: Opportunities Presented by the Energy Transition. European Association of Geoscientists and Engineers. 2018. (80th EAGE Conference and Exhibition 2018: Opportunities Presented by the Energy Transition).

Author

Piskarev, A. ; Kos'ko, M. / Westward progradation of Meso-Cenozoic tectonic deformations in the Laptev and East Siberian Seas region. 80th EAGE Conference and Exhibition 2018: Opportunities Presented by the Energy Transition. European Association of Geoscientists and Engineers, 2018. (80th EAGE Conference and Exhibition 2018: Opportunities Presented by the Energy Transition).

BibTeX

@inproceedings{18d47c34da574d968bf50b5e59e83127,
title = "Westward progradation of Meso-Cenozoic tectonic deformations in the Laptev and East Siberian Seas region",
abstract = "The gravity and magnetic anomalies, seismic and seismological data were analyzed to determine the nature and timing of tectonic deformations in the Laptev Sea and the western part of the East Siberian Sea. Formation of narrow elongated extensional structures (grabens) on the Laptev and East Siberian shelves may be attributed to different stages of evolution. This can occur due to westward shift of spreading activity in the Eurasian Basin which tentatively took place at Oligocene-Eocene interface (chron LMA 13) and in Pliocene. Direct geological observations in the marginal parts of one of the currently passive grabens on the shores of the Blagoveschensky Strait dividing the islands of Novaya Sibir{\textquoteright} and Faddeevsky make possible to determine the time line of deformation cessation in this area. A detailed combine analysis of different data made it possible to derive information on the tectonic events in the Laptev Sea – East Siberia Sea area. The main result is a tectonic subdivision of active deformation in present time the eastern Laptev Sea area and the western East Siberian Sea, where seismic and deformation activity took place from Cretaceous time and has finished in Pliocene.",
author = "A. Piskarev and M. Kos'ko",
year = "2018",
month = jan,
day = "1",
language = "English",
series = "80th EAGE Conference and Exhibition 2018: Opportunities Presented by the Energy Transition",
publisher = "European Association of Geoscientists and Engineers",
booktitle = "80th EAGE Conference and Exhibition 2018",
address = "Netherlands",
note = "80th EAGE Conference and Exhibition 2018: Opportunities Presented by the Energy Transition ; Conference date: 11-06-2018 Through 14-06-2018",

}

RIS

TY - GEN

T1 - Westward progradation of Meso-Cenozoic tectonic deformations in the Laptev and East Siberian Seas region

AU - Piskarev, A.

AU - Kos'ko, M.

PY - 2018/1/1

Y1 - 2018/1/1

N2 - The gravity and magnetic anomalies, seismic and seismological data were analyzed to determine the nature and timing of tectonic deformations in the Laptev Sea and the western part of the East Siberian Sea. Formation of narrow elongated extensional structures (grabens) on the Laptev and East Siberian shelves may be attributed to different stages of evolution. This can occur due to westward shift of spreading activity in the Eurasian Basin which tentatively took place at Oligocene-Eocene interface (chron LMA 13) and in Pliocene. Direct geological observations in the marginal parts of one of the currently passive grabens on the shores of the Blagoveschensky Strait dividing the islands of Novaya Sibir’ and Faddeevsky make possible to determine the time line of deformation cessation in this area. A detailed combine analysis of different data made it possible to derive information on the tectonic events in the Laptev Sea – East Siberia Sea area. The main result is a tectonic subdivision of active deformation in present time the eastern Laptev Sea area and the western East Siberian Sea, where seismic and deformation activity took place from Cretaceous time and has finished in Pliocene.

AB - The gravity and magnetic anomalies, seismic and seismological data were analyzed to determine the nature and timing of tectonic deformations in the Laptev Sea and the western part of the East Siberian Sea. Formation of narrow elongated extensional structures (grabens) on the Laptev and East Siberian shelves may be attributed to different stages of evolution. This can occur due to westward shift of spreading activity in the Eurasian Basin which tentatively took place at Oligocene-Eocene interface (chron LMA 13) and in Pliocene. Direct geological observations in the marginal parts of one of the currently passive grabens on the shores of the Blagoveschensky Strait dividing the islands of Novaya Sibir’ and Faddeevsky make possible to determine the time line of deformation cessation in this area. A detailed combine analysis of different data made it possible to derive information on the tectonic events in the Laptev Sea – East Siberia Sea area. The main result is a tectonic subdivision of active deformation in present time the eastern Laptev Sea area and the western East Siberian Sea, where seismic and deformation activity took place from Cretaceous time and has finished in Pliocene.

UR - http://www.scopus.com/inward/record.url?scp=85067923712&partnerID=8YFLogxK

M3 - Conference contribution

T3 - 80th EAGE Conference and Exhibition 2018: Opportunities Presented by the Energy Transition

BT - 80th EAGE Conference and Exhibition 2018

PB - European Association of Geoscientists and Engineers

T2 - 80th EAGE Conference and Exhibition 2018: Opportunities Presented by the Energy Transition

Y2 - 11 June 2018 through 14 June 2018

ER -

ID: 50073494