Structure of the Khatanga–Lomonosov Fracture Zone according to Seismic Data


Дәйексөз келтіру

Толық мәтін

Ашық рұқсат Ашық рұқсат
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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.

Авторлар туралы

E. Shipilov

Polar Geophysical Institute, Kola Science Center,
Russian Academy of Sciences

Хат алмасуға жауапты Автор.
Email: shipilov@pgi.ru
Ресей, Murmansk, 183010

L. Lobkovsky

Shirshov Institute of Oceanology, Russian Academy
of Sciences

Email: shipilov@pgi.ru
Ресей, Moscow, 117218

S. Shkarubo

Marine Arctic Geological Expedition

Email: shipilov@pgi.ru
Ресей, Murmansk, 183038

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© Pleiades Publishing, Ltd., 2019