Abstract: Change in anisotropic P-wave velocity observed by seafloor borehole observatory C0002G in the Nankai Trough subduction zone. (2015 AGU Fall Meeting)

Change in anisotropic P-wave velocity observed by seafloor borehole observatory C0002G in the Nankai Trough subduction zone.

Eiichiro Araki¹, Toshinori Kimura², Yuya Machida², Seiichi Miura³ and Shuichi Kodaira⁴, (1)Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Research Institute for Marine Geodynamics, Yokosuka, Japan, (2)JAMSTEC Japan Agency for Marine-Earth Science and Technology, Kanagawa, Japan, (3)JAMSTEC Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan, (4)Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokohama, Japan

Back to: Scientific Advances from Subduction Zone Observatories II