scholarly journals Temporal variations of crustal structure in the source region of the 2007 Noto Hanto Earthquake, central Japan, with passive image interferometry

2008 ◽  
Vol 60 (10) ◽  
pp. 1069-1074 ◽  
Author(s):  
Shiro Ohmi ◽  
Kazuro Hirahara ◽  
Hiroo Wada ◽  
Kiyoshi Ito
Keyword(s):  
Crustal Structure ◽  
Source Region ◽  
Temporal Variations ◽  
Central Japan ◽  
Noto Hanto Earthquake ◽  
2007 Noto Hanto Earthquake ◽  
Passive Image Interferometry

scholarly journals Coastal deformation associated with the 2007 Noto Hanto earthquake, central Japan, estimated from uplifted and subsided intertidal organisms

2008 ◽  
Vol 60 (10) ◽  
pp. 1059-1062 ◽  
Author(s):  
Yasuo Awata ◽  
Shinji Toda ◽  
Heitaro Kaneda ◽  
Takashi Azuma ◽  
Haruo Horikawa ◽  
...  
Keyword(s):  
Central Japan ◽  
Noto Hanto Earthquake ◽  
2007 Noto Hanto Earthquake

scholarly journals Magnetotelluric observations around the focal region of the 2007 Noto Hanto Earthquake (Mj 6.9), Central Japan

2008 ◽  
Vol 60 (2) ◽  
pp. 117-122 ◽  
Author(s):  
Ryokei Yoshimura ◽  
Naoto Oshiman ◽  
Makoto Uyeshima ◽  
Yasuo Ogawa ◽  
Masaaki Mishina ◽  
...  
Keyword(s):  
Focal Region ◽  
Central Japan ◽  
Noto Hanto Earthquake ◽  
2007 Noto Hanto Earthquake

scholarly journals Twin enigmatic microseismic sources in the Gulf of Guinea observed on intercontinental seismic stations

2013 ◽  
Vol 194 (1) ◽  
pp. 362-366 ◽  
Author(s):  
Yingjie Xia ◽  
Sidao Ni ◽  
Xiangfang Zeng
Keyword(s):  
North America ◽  
Temporal Variation ◽  
Crustal Structure ◽  
Source Region ◽  
Broad Band ◽  
Active Volcano ◽  
Gulf Of Guinea ◽  
Waveform Data ◽  
Seismic Stations ◽  
The Earth

Abstract Based on studies of continuous waveform data recorded on broad-band seismograph stations in Africa, Europe and North America, we report evidences for two temporally persistent and spatially localized monochromatic vibrating sources (around 0.036 and 0.038 Hz, respectively) in the Gulf of Guinea, instead of just one source (0.038 Hz or 26 s) found 50 yr ago. The location of the 0.036 Hz source is close to the Sao Tome Volcano, therefore it may be related to volcano processes. However, the 0.038 Hz source cannot be explained with known mechanisms, such as tectonic or oceanic processes. The most likely mechanism is volcano processes, but there is no reported active volcano in source region. Such repetitive vibration sources may provide valuable tools for detecting temporal variation of crustal structure of the Earth.

Configuration of subducting Philippine Sea plate and crustal structure in the central Japan region

2003 ◽  
Vol 30 (5) ◽  
pp. n/a-n/a ◽  
Author(s):  
T. Iidaka ◽  
T. Iwasaki ◽  
T. Takeda ◽  
T. Moriya ◽  
I. Kumakawa ◽  
...  
Keyword(s):  
Crustal Structure ◽  
Philippine Sea Plate ◽  
Central Japan ◽  
Philippine Sea

Configuration of subducting Philippine Sea plate and crustal structure in the central Japan region

2004 ◽  
Vol 388 (1-4) ◽  
pp. 7-20 ◽  
Author(s):  
Takashi Iidaka ◽  
Tetsuya Takeda ◽  
Eiji Kurashimo ◽  
Tomonori Kawamura ◽  
Yoshiyuki Kaneda ◽  
...  
Keyword(s):  
Crustal Structure ◽  
Philippine Sea Plate ◽  
Central Japan ◽  
Philippine Sea

scholarly journals Observation of ground motions of aftershocks of the 2007 Noto Hanto earthquake in Monzenmachi, the Wajima city, for estimation of site amplification

2008 ◽  
Vol 60 (10) ◽  
pp. 1063-1067 ◽  
Author(s):  
Hiroaki Yamanaka ◽  
Kentaro Motoki ◽  
Nobuyuki Yamada ◽  
Tatsuya Sugawara ◽  
Yumi Mabuchi ◽  
...  
Keyword(s):  
Ground Motions ◽  
Site Amplification ◽  
Noto Hanto Earthquake ◽  
2007 Noto Hanto Earthquake
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