T23D:
Bridging Tectonics and Earthquake Cycles IV

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Session ID#: 16023

Session Description:
Long-term tectonic processes shape the bulk of conditions under which faults operate and thereby influence earthquake processes on short time scales. In turn, rupture processes locally reduce the strength of the brittle lithosphere and thereby affect long-term processes. Reconciling observations of mechanisms taking place across these different time and spatial scales will improve our understanding of the rheology of the lithosphere-asthenosphere system and may ultimately improve seismic hazard assessment. What are the driving forces and the rheological structure at plate boundaries? What are the relative contributions of rheology (temperature, fluids, chemistry) and geometry in the segmentation of fault ruptures? What are the roles of faulting and off-fault deformation in shaping the landscape and partitioning seismic and aseismic energy dissipation? We seek contributions from across the fields of geology, geodynamics, seismology, and geodesy  involving both modelling and observational studies.
Primary Convener:  Sylvain Barbot, University of Southern California, Department of Earth Sciences, Los Angeles, CA, United States
Conveners:  Ylona van Dinther, Utrecht University, Department of Earth Sciences, Utrecht, Netherlands, Romain Jolivet, Ecole Normale Supérieure, PSL, CNRS UMR 8538, Laboratoire de Géologie, Département de Géosciences, Paris, France and Fabio Corbi, Deutsches GeoForschungsZentrum GFZ, Potsdam, Germany
Chairs:  Fabio Corbi, Deutsches GeoForschungsZentrum GFZ, Potsdam, Germany and Romain Jolivet, Ecole Normale Supérieure, PSL, CNRS UMR 8538, Laboratoire de Géologie, Département de Géosciences, Paris, France
OSPA Liaison:  Sylvain Barbot, University of Southern California, Department of Earth Sciences, Los Angeles, CA, United States

Cross-Listed:
  • G - Geodesy
  • S - Seismology

Abstracts Submitted to this Session:

Yehuda Ben-Zion, University of Southern California, Department of Earth Sciences and Statewide California Earthquake Center, Los Angeles, CA, United States and Vladimir Lyakhovsky, Geological Survey of Isreal, Jerusalem, Israel
Clément Perrin, Felix Waldhauser and Christopher H Scholz, Lamont-Doherty Earth Observatory, Palisades, NY, United States
Casper Cornelis Pranger, ETH Zurich, Institute of Geophysics, Zurich, Switzerland, Laetitia Le Pourhiet, LATMOS Laboratoire Atmosphères, Milieux, Observations Spatiales, Paris Cedex 05, France, Dave May, ETH Swiss Federal Institute of Technology Zurich, Zurich, Switzerland, Ylona van Dinther, Utrecht University, Department of Earth Sciences, Utrecht, Netherlands and Taras Gerya, ETH Zurich, Department of Earth and Planetary Sciences, Zurich, Switzerland
Kali L Allison, Stanford University, Stanford, CA, United States and Eric M Dunham, Stanford University, Institute for Computational and Mathematical Engineering, Stanford, CA, United States
Felipe Aron1,2, Nicolás Estay1,3, Jose M Cembrano1,4 and Gonzalo A Yanez1,4, (1)Pontifical Catholic University of Chile, Ingeniería Estructural y Geotécnica, Santiago, Chile, (2)Andean Geothermal Center of Excellence, Santiago, Chile, (3)Andean Geothermal Center of Excellence (CEGA), Santiago, Chile, (4)National Research Center for Integrated Natural Disasters Management (CIGIDEN), Santiago, Chile
Samer Naif, Lamont -Doherty Earth Observatory, Palisades, NY, United States and Dan Bassett, Scripps Institution of Oceanography, La Jolla, CA, United States
Marco Bohnhoff1, Patricia Martínez-Garzón1, Yehuda Ben-Zion2, Fatih Bulut3 and Eva Stierle1, (1)Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Potsdam, Germany, (2)University of Southern California, Los Angeles, CA, United States, (3)Bogazici University, Kandilli Observatory and ERI.-Department of Geodesy, Istanbul, Turkey

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