A fluid-rich layer along the Nankai trough megathrust fault off the Kii Peninsula inferred from receiver function inversion

2017 ◽  
Vol 122 (8) ◽  
pp. 6524-6537 ◽  
Author(s):  
Takeshi Akuhara ◽  
Kimihiro Mochizuki ◽  
Hitoshi Kawakatsu ◽  
Nozomu Takeuchi



2017 ◽  
Vol 69 (0) ◽  
pp. 59-68 ◽  
Author(s):  
Kenji NAKATA ◽  
Akio KOBAYASHI ◽  
Kenji HIRATA ◽  
Hiroaki TSUSHIMA ◽  
Akira YAMAZAKI ◽  
...  


Author(s):  
Serdar Ozalaybey ◽  
Martha K. Savage ◽  
Sushil J. Louis




2012 ◽  
Vol 55 (2) ◽  
pp. 194-205 ◽  
Author(s):  
Heng-Chu PENG ◽  
Jia-Fu HU ◽  
Hai-Yan YANG ◽  
Li-Min WEN


Author(s):  
Yoshiyuki Kaneda ◽  
Katsuyoshi Kawaguchi ◽  
Eiichiro Araki ◽  
Hiroyuki Matsumoto ◽  
Takeshi Nakamura ◽  
...  

The Nankai Trough is well known as the mega thrust earthquake generating tsunamis, with the interval of 100–150 years. The 1944 Tonankai and the 1946 Nankai earthquakes around the Nankai trough, each hypocenter was located off the Kii peninsula. Based on structural and simulation researches, we proposed and have been starting to deploy the dense ocean floor observatory network system around the Tonankai seismogenic zone, to monitor crustal activities using broadband seismometer, accelerometer and precise pressure gauges. The ocean floor network is significant ant important to monitor the crustal activities around mega-thrust earthquakes.



2013 ◽  
Vol 48 ◽  
pp. 106-122 ◽  
Author(s):  
Hugo Monsalve ◽  
Javier F. Pacheco ◽  
Carlos A. Vargas ◽  
Yorly A. Morales






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