Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Causes of Cretaceous Remagnetization on the Southwestern Periphery of the Archipelago of the New Siberian Islands. / Chernova, A. I.; Metelkin, D. V.; Vernikovsky, V. A. и др.
в: Doklady Earth Sciences, Том 481, № 1, 01.07.2018, стр. 847-851.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Causes of Cretaceous Remagnetization on the Southwestern Periphery of the Archipelago of the New Siberian Islands
AU - Chernova, A. I.
AU - Metelkin, D. V.
AU - Vernikovsky, V. A.
AU - Matushkin, N. Yu
PY - 2018/7/1
Y1 - 2018/7/1
N2 - This study demonstrates rock-magnetic and paleomagnetic investigations of Devonian and Mesozoic deposits of Kotelny, Stolbovoy, and Great Lyakhovsky islands. The results indicate that local remagnetization took place on the southwestern periphery on the archipelago of the New Siberian Islands. A comparison of new data with the apparent polar wander path for Siberia shows that the remagnetization happened during collisional events between 140 and 80 Ma and affected only the marginal part of the terrane of the New Siberian Islands that was directly facing the deformation front. The consistent younging of the remagnetization age from the south to the north indicates dextral rotation of the terrane of the New Siberian Islands during its collision with Siberia.
AB - This study demonstrates rock-magnetic and paleomagnetic investigations of Devonian and Mesozoic deposits of Kotelny, Stolbovoy, and Great Lyakhovsky islands. The results indicate that local remagnetization took place on the southwestern periphery on the archipelago of the New Siberian Islands. A comparison of new data with the apparent polar wander path for Siberia shows that the remagnetization happened during collisional events between 140 and 80 Ma and affected only the marginal part of the terrane of the New Siberian Islands that was directly facing the deformation front. The consistent younging of the remagnetization age from the south to the north indicates dextral rotation of the terrane of the New Siberian Islands during its collision with Siberia.
UR - http://www.scopus.com/inward/record.url?scp=85051193401&partnerID=8YFLogxK
U2 - 10.1134/S1028334X18070036
DO - 10.1134/S1028334X18070036
M3 - Article
AN - SCOPUS:85051193401
VL - 481
SP - 847
EP - 851
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
IS - 1
ER -
ID: 16075837