09:00 〜 09:15
[SCG45-11] Fault zone characterization using scattered waves recorded by distributed acoustic sensing
★Invited Papers
*Yan Yang1、James Atterholt1、Zhongwen Zhan1 (1.California Institute of Technology)
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[E] 口頭発表
セッション記号 S (固体地球科学) » S-CG 固体地球科学複合領域・一般
2023年5月25日(木) 09:00 〜 10:15 国際会議室 (IC) (幕張メッセ国際会議場)
コンビーナ:加藤 愛太郎(東京大学地震研究所)、山口 飛鳥(東京大学大気海洋研究所)、濱田 洋平(独立行政法人海洋研究開発機構 高知コア研究所)、Yihe Huang(University of Michigan Ann Arbor)、Chairperson:Lei YANG(Earthquake Research Institute, the University of Tokyo)、荒木 英一郎(海洋研究開発機構)
A growing evidence of geophysical observations has demonstrated that earthquake faults host a broad spectrum of slip modes from slow to unstable fast slip, which may lead to complexity in the nucleation process, rupture behavior, and slip & energy distribution. This discovery has boosted up vigorous discussions about the connection between slow and fast earthquakes including large earthquakes. How and when does a slow earthquake become a fast earthquake? To answer this fundamental question, it is particularly important to proceed further interdisciplinary research through the integration of geophysics, seismology, geodesy, geology, and physics. Developments of measurement technology, application of information science and statistical methods to seismic big-data and utilization of high-performance computing are required as key ingredients in accelerating the integration. This session encourages presentations shedding light on geophysical observations, data analysis, field studies, laboratory experiments, numerical modeling, and theoretical studies. We also welcome contributions from cutting-edge science and technology fields that explore development of novel measurements, data-driven analysis, and large-scale computation etc., those are relevant to slow and fast earthquakes.
09:00 〜 09:15
*Yan Yang1、James Atterholt1、Zhongwen Zhan1 (1.California Institute of Technology)
09:15 〜 09:30
09:30 〜 09:45
*Francisco H Ortega-Culaciati1、Marcos Moreno2、Hiroki Kawabata3、Shoichi Yoshioka4,3、Vicente Yañez-Cuadra5、Felipe Donoso5、Juan Carlos Báez6、Andrés Tassara7、Joaquin Hormazabal1 (1.Departamento de Geofísica, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Santiago, Chile.、2.Departamento de Ingeniería Estructural y Geotécnica, Pontificia Universidad Católica de Chile, Santiago, Chile.、3.Department of Planetology, Graduate School of Science, Kobe University, Rokkodai-cho 1-1, Nada Ward, Kobe 657-8501, Japan.、4.Research Center for Urban Safety and Security, Kobe University, Rokkodai-cho 1-1, Nada Ward, Kobe, 657-8501, Japan.、5.Departamento de Geofísica, Facultad de Ciencias Físicas y Matemáticas, Universidad de Concepción, Concepción, Chile.、6.Centro Sismológico Nacional, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Santiago, Chile.、7.Departamento de Geología, Facultad de Ciencias Químicas, Universidad de Concepción, Concepción, Chile)
09:45 〜 10:00
*Lei YANG1,2,3、Xin Liu4、Liang Zhao2、Weiqiang Zhu5、Gregory C. Beroza3 (1.Earthquake Research Institute, the University of Tokyo、2.Institute of Geology and Geophysics, Chinese Academy of Sciences、3.Department of Geophysics, Stanford University、4.University of Hong Kong、5.Department of Earth & Planetary Science, University of California)
10:00 〜 10:15