Structural Evidence of Recent Activity of the Khatanga–Lomonosov Fault Zone in the Laptev Sea
- Авторлар: Baranov B.V.1, Flint M.V.1, Rimskiy-Korsakov N.A.1, Poyarkov S.G.1, Dozorova K.A.1
-
Мекемелер:
- Shirshov Institute of Oceanology
- Шығарылым: Том 480, № 1 (2018)
- Беттер: 671-673
- Бөлім: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/193232
- DOI: https://doi.org/10.1134/S1028334X18050215
- ID: 193232
Дәйексөз келтіру
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.
Авторлар туралы
B. Baranov
Shirshov Institute of Oceanology
Хат алмасуға жауапты Автор.
Email: bbaranov@rambler.ru
Ресей, Moscow, 117218
M. Flint
Shirshov Institute of Oceanology
Email: bbaranov@rambler.ru
Ресей, Moscow, 117218
N. Rimskiy-Korsakov
Shirshov Institute of Oceanology
Email: bbaranov@rambler.ru
Ресей, Moscow, 117218
S. Poyarkov
Shirshov Institute of Oceanology
Email: bbaranov@rambler.ru
Ресей, Moscow, 117218
K. Dozorova
Shirshov Institute of Oceanology
Email: bbaranov@rambler.ru
Ресей, Moscow, 117218
Қосымша файлдар
