NH53C:
Toward a Unified and Worldwide Database of Earthquake Surface Ruptures II Posters

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Session ID#: 13523

Session Description:
The session will address issues related to surface rupture hazard which can result in damage to structures located nearby active faults. Recent earthquakes have shown that distributed surface faulting can be of engineering significance, even for moderate quakes. In the probabilistic approach (PFDHA), the attenuation term describing the decrease of displacement with distance is based on sparsely populated databases. There is thus a need to build a worldwide, unified and standardized dataset with an improved spatial completeness and a broad magnitude range.  We encourage contributions that provide field data on earthquake ruptures, explore the impact of "site-specific" conditions such as surficial geology, develop remote sensing techniques to enrich the dataset based on classical field measurements, and present how uncertainties are treated. This session is proposed in the framework of INQUA and IAEA projects with the aim of using the updated database for a robust calibration of PFDHA attenuation parameters.
Primary Convener:  Stéphane Baize, IRSN Institut de Radioprotection et de Sûreté Nucléaire, Fontenay Aux Roses Cedex, France
Conveners:  Timothy E Dawson, California Geological Survey, San Mateo, CA, United States, Makoto Takao, Tokyo Electric Power Company Holdings, Inc., TEPCO - Research Institute, Tokyo, Japan and Katsunori Sugaya, Nuclear Regulation Authority, Regulatory Standard and Research, Tokyo, Japan
Chairs:  Stéphane Baize, IRSN Institut de Radioprotection et de Sûreté Nucléaire, Fontenay Aux Roses Cedex, France and Timothy E Dawson, California Geological Survey, San Mateo, CA, United States
OSPA Liaison:  Timothy E Dawson, California Geological Survey, San Mateo, CA, United States
Index Terms:

Abstracts Submitted to this Session:

Yoshimitsu Fukushima, Organization Not Listed, Washington, DC, United States
Naoto Inoue1, Naoko Kitada1 and Masao Tonagi2, (1)Geo-Research Institute, Osaka, Japan, (2)Kozo Keikaku Engineering Inc., Tokyo, Japan
Naoko Kitada1, Naoto Inoue1 and Masao Tonagi2, (1)Geo-Research Institute, Osaka, Japan, (2)Kozo Keikaku Engineering Inc., Tokyo, Japan
Masao Tonagi1, Tsutomu Takahama1, Yasuhiro Matsumoto1, Naoto Inoue2, Kojiro Irikura3 and Luis Angel Dalguer3, (1)Kozo Keikaku Engineering Inc., Tokyo, Japan, (2)Geo-Research Institute, Osaka, Japan, (3)Aichi Institute of Technology, Toyota, Japan
Liang Chun Wu1, Chien Hung Li2 and M. L. Lin1, (1)National Taiwan University, Taipei, Taiwan, (2)National Taiwan University, Department of Civil Engineering, Taipei, Taiwan
Chien Hung Li1, Liang Chun Wu2, PEI Chen Chan2 and M. L. Lin2, (1)National Taiwan University, Department of Civil Engineering, Taipei, Taiwan, (2)National Taiwan University, Taipei, Taiwan
Yi-Kai Lin1, Ming Chun Ke1 and Siao-Syun Ke2, (1)NCDR National Science and Technology Center for Disaster Reduction of Taiwan, New Taipei, Taiwan, (2)National Science and Technology Center for Disaster Reduction, New Taipei City, Taiwan
Rodrigo Alejandro León Loya1, Pierre Lacan1, Maria Ortuňo2, Hernández Ana Paula3, Petra Štěpančíková4, Jakub Stemberk5, Ramon Ramón Zuniga1 and Gerardo J Aguirre-Diaz1, (1)Centro de Geociencias, UNAM, Juriquilla, Queretaro, Mexico, (2)Faculty of Geology, University of Barcelona, Department of Geodynamics and Physics, Barcelona, Spain, (3)Centro de Investigación Científica y de Educación Superior de Ensenada, Ciencias de la Tierra, San Diego, CA, United States, (4)Czech Academy of Sciences, Institute of Rock Structure and Mechanics, Prague, Czech Republic, (5)Academy of Sciences of the Czech Republic, Institute of Rock Structure and Mechanics, Department of Neotectonics and Thermochronology, Prague, Czech Republic
Esther Hintersberger and Kurt Decker, University of Vienna, Vienna, Austria

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