Fig. 1 Postseismic displacements recorded by land and seafloor GPS sites from September 2012 to May 2016 after the 2011 Mw 9.0 Tohoku earthquake. Postseismic.

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Spatial-temporal pattern of lower-crustal effective viscosities

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Presentation transcript:

Fig. 1 Postseismic displacements recorded by land and seafloor GPS sites from September 2012 to May 2016 after the 2011 Mw 9.0 Tohoku earthquake. Postseismic displacements recorded by land and seafloor GPS sites from September 2012 to May 2016 after the 2011 Mw 9.0 Tohoku earthquake. (A) Postseismic displacement field and location of the modeled transect (thick black line). Gray and white arrows indicate horizontal motions recorded by GEONET (Geospatial Information Authority of Japan) and Tohoku University/Japan Coast Guard instruments, respectively. Colors indicate vertical motions: red-blue shading for inland motion and colored circles for ocean bottom motion. Black-yellow contours in the seafloor indicate the coseismic slip distribution estimated from land and seafloor geodetic data [GPS/A; ocean bottom pressure gauge (OBP); (14)]. Red triangles indicate Quaternary volcanoes. Black dots indicate the site locations for time series: Oshika, Naruko, and Toyoura from east to west. (B) Two-dimensional displacement along the transect from September 2012 to May 2016. Black and red show horizontal and vertical displacements, respectively. (C) Time series of GPS displacements at the selected locations: Oshika station at the forearc, Naruko station at the volcanic front, and Toyoura station at the backarc. (D) Subduction zone thermal structure (53). (E) Steady-state viscosity structure calculated using the thermal structure (D). J. Muto et al. Sci Adv 2019;5:eaaw1164 Copyright © 2019 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).