Abstract: Continuous Shear Wave Signals from around a Subducted Seamount Following 2014 Mw 6.8 Slow-slip Event in the Hikurangi Subduction Margin Offshore New Zealand (2017 AGU Fall Meeting)

Continuous Shear Wave Signals from around a Subducted Seamount Following 2014 Mw 6.8 Slow-slip Event in the Hikurangi Subduction Margin Offshore New Zealand

Yuriko Iwasaki¹, Kimihiro Mochizuki¹, Motoko Ishise¹, Erin K Todd², Susan Y Schwartz³, Stuart A Henrys⁴, Martha K Savage⁵, Anne Sheehan⁶, Yoshihiro Ito⁷, Laura M Wallace⁸, Spahr C Webb⁹, Hubert Jerzy Zal¹⁰, Tomoaki Yamada¹ and Masanao Shinohara¹¹, (1)Earthquake Research Institute, The University of Tokyo, Tokyo, Japan, (2)University of Otago, Dunedin, New Zealand, (3)University of California Santa Cruz, Earth and Planetary Sciences, Santa Cruz, CA, United States, (4)GNS Science, Lower Hutt, New Zealand, (5)Victoria University of Wellington, Wellington, New Zealand, (6)University of Colorado Boulder, Cooperative Institute for Research in Environmental Sciences, Boulder, United States, (7)Disaster Prevention Research Institute, Kyoto University, Kyoto, Japan, (8)University of Texas, Institute for Geophysics, Austin, United States, (9)Lamont-Doherty Earth Observatory, Palisades, NY, United States, (10)Victoria University of Wellington, School of Geography, Environment and Earth Sciences, Wellington, New Zealand, (11)National Research Institute for Earth Science and Disaster Resilience/Earthquake Research Institute, The University of Tokyo, Tokyo, Japan

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