Structure of the Khatanga–Lomonosov Fracture Zone according to Seismic Data
- Авторы: Shipilov E.V.1, Lobkovsky L.I.2, Shkarubo S.I.3
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Учреждения:
- Polar Geophysical Institute, Kola Science Center, Russian Academy of Sciences
- Shirshov Institute of Oceanology, Russian Academy of Sciences
- Marine Arctic Geological Expedition
- Выпуск: Том 487, № 1 (2019)
- Страницы: 846-851
- Раздел: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/195281
- DOI: https://doi.org/10.1134/S1028334X19070286
- ID: 195281
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Аннотация
Based on the results of geophysical data interpretation, the structural features of the Khatanga–Lomonosov fracture zone (KhLZ), adapted to the junction zone between the Laptev Sea continental margin and structures of the Eurasian spreading basin and the Lomonosov Ridge, are considered. The KhLZ reflection in anomalous geophysical fields and in wave seismic patterns observed in the sections is shown on the example of separate links, and also the character of its kinematic interrelations with heterogeneous tectonic elements is illustrated. The tectonic nature and the role played by this fault zone in the geodynamic evolution of the region are substantiated.
Об авторах
E. Shipilov
Polar Geophysical Institute, Kola Science Center,Russian Academy of Sciences
Автор, ответственный за переписку.
Email: shipilov@pgi.ru
Россия, Murmansk, 183010
L. Lobkovsky
Shirshov Institute of Oceanology, Russian Academyof Sciences
Email: shipilov@pgi.ru
Россия, Moscow, 117218
S. Shkarubo
Marine Arctic Geological Expedition
Email: shipilov@pgi.ru
Россия, Murmansk, 183038
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