Structural Evidence of Recent Activity of the Khatanga–Lomonosov Fault Zone in the Laptev Sea
- Авторы: Baranov B.V.1, Flint M.V.1, Rimskiy-Korsakov N.A.1, Poyarkov S.G.1, Dozorova K.A.1
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Учреждения:
- Shirshov Institute of Oceanology
- Выпуск: Том 480, № 1 (2018)
- Страницы: 671-673
- Раздел: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/193232
- DOI: https://doi.org/10.1134/S1028334X18050215
- ID: 193232
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Аннотация
New structural data obtained by a geophysical survey during Cruise 69 of the R/V Akademik Mstislav Keldysh in 2017 indicate that the Khatanga−Lomonosov fault zone is presently active and propagating in Khatanga Bay. The orientation of conjugated extension and compression structures points to the sinistral displacement along this zone. The results confirm the concept that this zone represents a transform fault separating Gakkel Ridge from the rift system of the Laptev Sea shelf.
Об авторах
B. Baranov
Shirshov Institute of Oceanology
Автор, ответственный за переписку.
Email: bbaranov@rambler.ru
Россия, Moscow, 117218
M. Flint
Shirshov Institute of Oceanology
Email: bbaranov@rambler.ru
Россия, Moscow, 117218
N. Rimskiy-Korsakov
Shirshov Institute of Oceanology
Email: bbaranov@rambler.ru
Россия, Moscow, 117218
S. Poyarkov
Shirshov Institute of Oceanology
Email: bbaranov@rambler.ru
Россия, Moscow, 117218
K. Dozorova
Shirshov Institute of Oceanology
Email: bbaranov@rambler.ru
Россия, Moscow, 117218
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