Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Early Paleozoic tectonics for the New Siberian Islands terrane (Eastern Arctic). / Metelkin, D. V.; Chernova, A. I.; Vernikovsky, V. A. и др.
в: Doklady Earth Sciences, Том 477, № 1, 01.11.2017, стр. 1277-1281.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Early Paleozoic tectonics for the New Siberian Islands terrane (Eastern Arctic)
AU - Metelkin, D. V.
AU - Chernova, A. I.
AU - Vernikovsky, V. A.
AU - Matushkin, N. Yu
PY - 2017/11/1
Y1 - 2017/11/1
N2 - The New Siberian Islands archipelago is one of the few research objects accessible for direct study on the eastern Arctic shelf. There are several models that have different interpretations of the Paleozoic tectonic history and the structural affinity of the New Siberian Islands terrane. Some infer a direct relationship with the passive continental margin of the Siberian paleocontinent. Others connect it with the marginal basins of Baltica and Laurentia, or the Chukotka-Alaska microplate. Our paleomagnetic investigation led us to create an apparent polar wander path for the early Paleozoic interval of geological history. Based on it we can conclude that the New Siberian Islands terrane could not have been a part of these continental plates. This study considers the possible tectonic scenarios of the Paleozoic history of the Earth, presents and discusses the corresponding global reconstructions describing the paleogeography and probable mutual kinematics of the terranes of the Eastern Arctic.
AB - The New Siberian Islands archipelago is one of the few research objects accessible for direct study on the eastern Arctic shelf. There are several models that have different interpretations of the Paleozoic tectonic history and the structural affinity of the New Siberian Islands terrane. Some infer a direct relationship with the passive continental margin of the Siberian paleocontinent. Others connect it with the marginal basins of Baltica and Laurentia, or the Chukotka-Alaska microplate. Our paleomagnetic investigation led us to create an apparent polar wander path for the early Paleozoic interval of geological history. Based on it we can conclude that the New Siberian Islands terrane could not have been a part of these continental plates. This study considers the possible tectonic scenarios of the Paleozoic history of the Earth, presents and discusses the corresponding global reconstructions describing the paleogeography and probable mutual kinematics of the terranes of the Eastern Arctic.
UR - http://www.scopus.com/inward/record.url?scp=85037160724&partnerID=8YFLogxK
U2 - 10.1134/S1028334X17110228
DO - 10.1134/S1028334X17110228
M3 - Article
AN - SCOPUS:85037160724
VL - 477
SP - 1277
EP - 1281
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 1
ER -
ID: 9067394