A very long-term transient event preceding the 2011 Tohoku earthquake
نویسندگان
چکیده
منابع مشابه
The 2011 Tohoku earthquake and devastating tsunami.
At 14:46 on March 11, 2011, the magnitude-9.0 earthquake attacked Sendai and neighboring cities distributed along the northeast coast of Honshu Island, Japan. Its epicenter is located 130 km east of Sendai (Fig. 1). Unfortunate ly, the strong earthquake generated devastating tsunamis that destroyed many towns and villages near the seashore in Iwate, Miyagi, and Fukushima prefectures. The natura...
متن کاملRecurrent slow slip event likely hastened by the 2011 Tohoku earthquake.
Slow slip events (SSEs) are another mode of fault deformation than the fast faulting of regular earthquakes. Such transient episodes have been observed at plate boundaries in a number of subduction zones around the globe. The SSEs near the Boso Peninsula, central Japan, are among the most documented SSEs, with the longest repeating history, of almost 30 y, and have a recurrence interval of 5 to...
متن کاملThe psychosocial response to the 2011 Tohoku earthquake.
Alındığı Tarih: 24.08.2012 Kabul Tarihi: 7.12.2012 Yazışma adresi: World Health Organization WHO Press 20 Avenue Appia, Office 4152 CH 1211 Geneve 27, Switzerland e-posta: [email protected] [email protected] On 11 March 2011, an earthquake with a magnitude of 9.0 on the Richter scale struck off the coast of Japan, triggering destructive tsunami waves of up to 40 metres high that swept over ...
متن کاملDisplacement above the hypocenter of the 2011 Tohoku-Oki earthquake.
The moment magnitude (M(w)) = 9.0 2011 Tohoku-Oki mega-thrust earthquake occurred off the coast of northeastern Japan. Combining Global Positioning System (GPS) and acoustic data, we detected very large sea-floor movements associated with this event directly above the focal region. An area with more than 20 meters of horizontal displacement, that is, four times larger than those detected on lan...
متن کاملPrompt gravity signal induced by the 2011 Tohoku-Oki earthquake
Transient gravity changes are expected to occur at all distances during an earthquake rupture, even before the arrival of seismic waves. Here we report on the search of such a prompt gravity signal in data recorded by a superconducting gravimeter and broadband seismometers during the 2011 Mw 9.0 Tohoku-Oki earthquake. During the earthquake rupture, a signal exceeding the background noise is obs...
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ژورنال
عنوان ژورنال: Nature Communications
سال: 2015
ISSN: 2041-1723
DOI: 10.1038/ncomms6934