Research output: Contribution to journal › Article › peer-review
Paleozoic Tectonics and Geodynamics of the De Long Islands and Adjacent Structures of the Verkhoyansk-Chukotka Fold Belt. / Metelkin, D. V.; Chernova, A. I.; Matushkin, N. Yu et al.
In: Doklady Earth Sciences, Vol. 495, No. 1, 11.2020, p. 803-807.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Paleozoic Tectonics and Geodynamics of the De Long Islands and Adjacent Structures of the Verkhoyansk-Chukotka Fold Belt
AU - Metelkin, D. V.
AU - Chernova, A. I.
AU - Matushkin, N. Yu
AU - Vernikovsky, V. A.
N1 - Funding Information: This work was financially supported by the Russian Science Foundation (project no. 19-17-00091) and the Russian Foundation for Basic Research (projects nos. 18-05-70035, 18-05-00234, 20-05-00360). Publisher Copyright: © 2020, Pleiades Publishing, Ltd. Copyright: Copyright 2020 Elsevier B.V., All rights reserved.
PY - 2020/11
Y1 - 2020/11
N2 - This work presents finalized results of our paleomagnetic study of Paleozoic rocks of Henrietta, Jeannette and Bennett islands and their implications for tectonic reconstructions. We discuss possible relationships of the Cambrian section of the De Long sedimentary basin with the Verkhoyansk margin of Siberia, the terranes of the Kolyma-Omolon group, the Chukotka-Alaska microcontinent, as well as with the structures of the submerged Mendeleev Ridge. We propose a new tectonic model, in which the De Long structures feature as the frontalmost part of a large transform system that existed on the periphery of the Siberian paleocontinent.
AB - This work presents finalized results of our paleomagnetic study of Paleozoic rocks of Henrietta, Jeannette and Bennett islands and their implications for tectonic reconstructions. We discuss possible relationships of the Cambrian section of the De Long sedimentary basin with the Verkhoyansk margin of Siberia, the terranes of the Kolyma-Omolon group, the Chukotka-Alaska microcontinent, as well as with the structures of the submerged Mendeleev Ridge. We propose a new tectonic model, in which the De Long structures feature as the frontalmost part of a large transform system that existed on the periphery of the Siberian paleocontinent.
KW - Arctic
KW - Arctida
KW - De Long archipelago
KW - New Siberian Islands
KW - paleomagnetism
KW - paleotectonic reconstructions
UR - http://www.scopus.com/inward/record.url?scp=85097833755&partnerID=8YFLogxK
U2 - 10.1134/S1028334X20110100
DO - 10.1134/S1028334X20110100
M3 - Article
AN - SCOPUS:85097833755
VL - 495
SP - 803
EP - 807
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 1
ER -
ID: 27119758