Plate boundaries in the Far East region of Russia (from GPS measurement, seismic-prospecting, and seismological data)


статья в журнале
Авторы: Timofeev V.Y.   (ИНГГ СО РАН)   Ardyukov D.G.   (ИНГГ СО РАН)   Boiko E.V.   (ИНГГ СО РАН)   Timofeev A.V.   (ИНГГ СО РАН)   Solov'ev V.M.   (ИНГГ СО РАН)   Shibaev S.V.     Petrov A.F.     Gornov P.Y.     Shestakov N.V.    
дата публикации: 2012
реферат:
The recent geodynamics of the Far East region of Russia is considered, where three large tectonic plates converge-Eurasian, North American, and Pacific, as well as several microplates-Okhotsk, Bering, and Amurian-have been hypothesized to exist. The available data on the position of the plate boundaries, the relative plate rotation poles, and the regional seismicity were analyzed, and parameters of plate motion models for northeastern Russia were determined in this study. The regional deep structure was investigated, using data obtained by different geophysical methods. The results of observations of the Magadan-Vrangel Island profile by deep seismic sounding (DSS), common-depth point (CDP) method, and correlation refraction method (CRM) are presented. (C) 2012, V.S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.
первоисточник: Russian Geology and Geophysics
том: 4
страницы: 376-391
ISBN:
ISSN:
внешние ссылки:
WoS   WoS (цитирование)
DOI  
РИНЦ SPIN  
Scopus  

 Видео

 

 

 

 

полный текст статьи

rgg-2012-04-376