Kinematic inversion of postseismic deformation following the 2016 Mw 7.0 Kumamoto earthquake for the distribution of brittle and ductile crustal processes.
James Daniel Paul Moore1, Sylvain Barbot2, Valere Lambert3, Chi-Hsien Tang4, Dongju Peng1, Sagar Shrishailappa Masuti1, Justin Dauwels5, Songwei Wu5, Hang Yu5, Ya-Ju Hsu6, Priyamvada Nanjundiah1, Shengji Wei7, Eric Ostrom Lindsey8, Lujia Feng7, Bunichiro Shibazaki9 and Teng Wang10, (1)Earth Observatory of Singapore, Singapore, Singapore, (2)University of Southern California, Department of Earth Sciences, Los Angeles, CA, United States, (3)California Institute of Technology, Seismological Laboratory, Pasadena, United States, (4)Institute of Earth Sciences, Academia Sinica, Taipei, Taiwan, Taipei, Taiwan, (5)Nanyang Technological University, School of Electrical & Electronic Engineering, Singapore, Singapore, (6)Institute of Earth Sciences, Academia Sinica, Taipei, Taiwan, (7)Earth Observatory of Singapore, Nanyang Technological University, Singapore, Singapore, (8)Nanyang Technological University, Earth Observatory of Singapore, Singapore, Singapore, (9)Building Research Institute, Ibaraki, Japan, (10)Southern Methodist University, Dallas, TX, United States
