T31C:
The Mechanism of Tectonic Tremor II Posters


Session ID#: 10772

Session Description:
Low and very low frequency earthquakes detected within tectonic tremor bursts suggest brittle shear failure occurs at the source of tremor. Tremor occurs on subduction and transform plate boundaries and at a variety of depths. Grain scale deformation mechanisms may vary at these different locations, yet tremor is observed to have similar seismological characteristics. The physical conditions and processes that drive transitional behavior in mixed rheology deformation may be key to understanding whether there are common mechanisms at the source of tremor. In this session, we hope to include seismological observations, geological constraints, and insights from modeling and experiments to encourage an extensive review of tremor source processes. We also invite studies of microseismicity, repeating earthquakes and other phenomena in transitional fault regions that may shed light on the mechanisms of tremors and their implications for earthquake nucleation processes.
Primary Convener:  James D Kirkpatrick, McGill University, Earth & Planetary Sciences, Montreal, Canada
Conveners:  Whitney M Behr, Structural Geology and Tectonics Group, Geological Institute, Zurich, Switzerland, David R Shelly, USGS National Earthquake Information Center, Golden, United States and Jean Paul Ampuero, California Institute of Technology, Seismological Laboratory, Pasadena, CA, United States
Chairs:  James D Kirkpatrick, McGill University, Earth & Planetary Sciences, Montreal, Canada, Whitney M Behr, Structural Geology and Tectonics Group, Geological Institute, Zurich, Switzerland, David R Shelly, U.S. Geological Survey, Geologic Hazards Science Center, Golden, United States and Jean Paul Ampuero, California Institute of Technology, Seismological Laboratory, Pasadena, CA, United States
OSPA Liaison:  James D Kirkpatrick, McGill University, Earth & Planetary Sciences, Montreal, Canada

Cross-Listed:
  • MR - Mineral and Rock Physics
  • S - Seismology

Abstracts Submitted to this Session:

Alexandre P Plourde, Dalhousie University, Department of Earth and Environmental Sciences, Halifax, NS, Canada and Michael G Bostock, University of British Columbia, Vancouver, BC, Canada
Wen-Yen Chang, National Applied Research Laboratories, Taipei, Taiwan, Wei-Fang Sun, National Dong Hwa University, Department of Natural Resources and Environmental Studies, Hualien County, Taiwan and Hsin-Yuan Chen, National Dong Hwa University, Hualien County, Taiwan
James D Kirkpatrick, McGill University, Earth & Planetary Sciences, Montreal, Canada, Katharine Compton, Colorado State University, Fort Collins, CO, United States and Gregory J. Holk, California State University Long Beach, Long Beach, CA, United States
John G Armbruster, Columbia University of New York, Palisades, NY, United States
Nori Nakata, Lawrence Berkeley National Laboratory, Earth and Environmental Sciences Area, Berkeley, United States, Gregory C Beroza, Stanford University, Department of Geophysics, Stanford, CA, United States and Victor M Cruz-Atienza, Universidad Nacional Autonoma de Mexico, Mexico City, Mexico
Andres Felipe Felipe Peña Castro, McGill University, Montreal, QC, Canada, Rebecca M Harrington, Ruhr University Bochum, Institute of Geology, Mineralogy and Geophysics, Bochum, Germany and Elizabeth S Cochran, Organization Not Listed, Washington, DC, United States
Julie Maury1, Satoshi Ide2, Victor M Cruz-Atienza3, Vladimir Kostoglodov4 and Xyoli Perez-Campos4, (1)University of Tokyo, Bunkyo-ku, Japan, (2)The University of Tokyo, Department of Earth and Planetary Science, Bunkyo-ku, Japan, (3)Universidad Nacional Autonoma de Mexico, Mexico City, Mexico, (4)UNAM National Autonomous University of Mexico, Mexico City, Mexico
Natalia Poiata1, Claudio Satriano2, Jean-Pierre Vilotte1, Pascal Bernard3 and Kazushige Obara4, (1)Institut de Physique du Globe de Paris, Paris, France, (2)Université Paris Cité, Institut de physique du globe de Paris, Sismologie, Paris, France, (3)Institut de Physique du Globe de Paris (IPGP), Université Paris Cité, Paris, France, (4)The University of Tokyo, Earthquake Research Institute, Tokyo, Japan
Shelley Chestler1, Kenneth Creager1 and Abhijit Ghosh2, (1)Univ Washington, Seattle, WA, United States, (2)University of California Riverside, Riverside, CA, United States
Jiancang Zhuang, Institute of Statistical Mathematics, Tokyo, Japan, Ting Wang, University of Otago, Dunedin, New Zealand, Kazushige Obara, The University of Tokyo, Earthquake Research Institute, Tokyo, Japan and Hiroshi Tsuruoka, University of Tokyo, Bunkyo-ku, Japan

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