The 2006 (Мw 8.3) and 2007 (Мw 8.1) Simushir Earthquakes and the 2011 Tohoku Megaearthquake (Мw 9.0): Tectonic Stresses and Development of the Seismic Process
- 作者: Zlobin T.K.1
-
隶属关系:
- Institute of Marine Geology and Geophysics, Far East Branch
- 期: 卷 480, 编号 1 (2018)
- 页面: 599-601
- 栏目: Geophysics
- URL: https://ogarev-online.ru/1028-334X/article/view/193083
- DOI: https://doi.org/10.1134/S1028334X18050100
- ID: 193083
如何引用文章
详细
The peculiarities of catastrophic earthquakes that occurred in the Northwest Pacific region on January 13, 2007, and January 15, 2007, east of the Kuril Islands and the Tohoku megaearthquake of March 11, 2011, east of Japan are considered and analyzed. It is revealed that these earthquakes, apart from the fact that they occurred in the transition zone from the Pacific to island arcs and the Eurasian continent, have common features and similar characteristics. The seismotectonic slip in the source of the chronologically first event, the 2006 Kuril earthquake, was a gentle thrust, while that of the second event of January 13, 2007, was a downthrow beneath the Kuril deep trench.
作者简介
T. Zlobin
Institute of Marine Geology and Geophysics, Far East Branch
编辑信件的主要联系方式.
Email: t.zlobin@mail.ru
俄罗斯联邦, Yuzhno-Sakhalinsk, 693010
补充文件
