Recent geodynamics of the Kuril subduction zone


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Abstract

The collected GPS/GLONASS data allow us to reveal new information on the recent geodynamics of the Kuril Island arc. The maximum deformation stress accumulates in the southern and northern parts of the study area, while a long fading transition process of postseismic motions is observed in the central segment of the Kuril arc as a result of the 2006–2007 great Simushir earthquakes of Mw = 8.3 and Mw = 8.1. We have succeeded in revealing the recent interplate coupling geometry of the Pacific and the North American lithospheric plates and also in estimating the seismic potential of different segments of the Kuril subduction zone.

About the authors

A. S. Prytkov

Institute of Marine Geology and Geophysics, Far East Branch

Author for correspondence.
Email: nauka@imgg.ru
Russian Federation, ul. Nauki 1B, Yuzhno-Sakhalinsk, 693022

N. F. Vasilenko

Institute of Marine Geology and Geophysics, Far East Branch

Email: nauka@imgg.ru
Russian Federation, ul. Nauki 1B, Yuzhno-Sakhalinsk, 693022

D. I. Frolov

Ioffe Institute

Email: nauka@imgg.ru
Russian Federation, ul. Politekhnicheskaya 26, Saint Petersburg, 194021


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