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


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详细

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.

作者简介

E. Shipilov

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

编辑信件的主要联系方式.
Email: shipilov@pgi.ru
俄罗斯联邦, Murmansk, 183010

L. Lobkovsky

Shirshov Institute of Oceanology, Russian Academy
of Sciences

Email: shipilov@pgi.ru
俄罗斯联邦, Moscow, 117218

S. Shkarubo

Marine Arctic Geological Expedition

Email: shipilov@pgi.ru
俄罗斯联邦, Murmansk, 183038

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