[E] Poster
S (Solid Earth Sciences ) » S-SS Seismology
convener:Luca Urpi, Yusuke Mukuhira(Institute of Fluid Science, Tohoku University), Bogdan Enescu(Department of Geophysics, Kyoto University), Francesco Grigoli(ETH Zurich Swiss Federal Institute of Technology Zurich)
Induced and triggered seismicity occurs in conjunction with human activities such as reservoir impoundments, mining operations, conventional and non-conventional hydrocarbon production, geothermal energy exploitation, wastewater disposal, CO2 sequestration and gas storage operations as well as volcanic and hydrogeological processes. The stability of faults is affected by external solicitations such as pore-pressure diffusion, relaxation effects as well as perturbations related to mass, pressure, temperature and/or volume changes, dike intrusions and earthquake-earthquake interactions. A better understanding of the physical processes governing induced and triggered seismicity is important for the assess the risk of current and future industrial activities.
The study of induced and triggered seismicity is inherently an interdisciplinary problem, which requires the combination of seismological, hydrogeological, geodetic data and a wide range of modeling approaches. This session welcome contributions covering the analysis and modeling of induced and triggered seismicity at different spatial scales and environments.
Relevant topics to be presented include but are not limited to induced seismicity characterization, spatio-temporal variations of physical parameters (including stress, pressure and temperature changes), spatio-temporal patterns of seismicity, modeling strategies and case-studies.
The goal of the session is to cover both theoretical, numerical and experimental aspects of these topics.
*Yusuke Mukuhira1, Martin Ziegler2, Takatoshi Ito1, Hiroshi Asanuma3, Markus O Häring4 (1.Institute of Fluid Science, Tohoku University, 2.Department of Earth Sciences, Engineering Geology, ETH Zurich, 3.AIST, 4.Häring GeoProject)
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*Xu Chang1,2, Han Li1,2, Xiao-Bi Xie3 (1.Institute of Geology and Geophysics, Chinese Academy of Sciences, 2.Innovation Academy for Earth Sciences, Chinese Academy of Sciences, 3.University of California, Santa Cruz)
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*Kangnan Yan1,2, Yusuke Mukuhira1, Takatoshi Ito1, Yinhui Zuo2, Hiroshi Asanuma3, Markus O Häring4 (1.Institute of Fluid Science, Tohoku University, 2.State Key Laboratory of Oil and Gas Geology and Exploitation, Chengdu University of Technology, 3.Fukushima Renewable Energy Institute (FREA), National Institute of Advanced Industrial Science and Technology (AIST), 4.Häring GeoProject)
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*Calvin Luiramo Qwana1, Masatoshi Miyazawa1, James Mori1 (1.Disaster Prevention Research Institute Kyoto University )
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*Osamu Murakami1, Yasuhiro Asai1, Hiroshi Ishii1 (1.Tono Rearch Institute of Earthquake Science, Association for the Development of Earthquake Prediction)
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*Sheldon Dwight Warden1, Pascal Sailhac2, Stéphane Garambois3 (1.Hyperion Geophysical Services, 7 rue de Châtenois, 67100, Strasbourg, France., 2.GEOPS (Geosciences Paris Sud), Université de Paris Saclay, 15 Rue Georges Clemenceau, 91400, Orsay, France., 3.ISTerre (Institut des Sciences de la Terre), Université de Grenoble Alpes, 1381 rue de la piscine, 38400, Saint Martin d'Heres, France.)
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*Rezkia Dewi Andajani1, Takeshi Tsuji1,2 (1.Department of Earth Resources Engineering, Kyushu University , 2.International Institute for Carbon-Neutral Energy Research, Kyushu University)
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*Maita Eri1, Jiancang Zhuang (1.SOKENDAI)
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