G41A:
Geodetic Imaging and Interpretation of the Seismic Cycle I

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Session ID#: 30614

Session Description:
Geodesy’s ability to image earth processes has vastly improved both spatially and temporally in recent decades, making it an essential tool to study the seismic cycle and the ways the earth accommodates tectonic strain. To use geodesy to image these processes in a complex earth, it is essential to 1) correctly separate the contributions made by seismic, aseismic and nontectonic deformation in the data, and then 2) link these observations to fault and bulk processes with a full view of their spatiotemporal complexities. We welcome studies on all aspects of geodetic imaging of the seismic cycle: from improved techniques to detect tectonic signals (e.g. probabilistic, sparsity-promoting, etc.) and separate them from other deformation sources (e.g. hydrological, thermoelastic, anthropogenic), to the modeling and interpretation of the deformation mechanisms that produce them (e.g. coseismic slip, afterslip, viscoelastic relaxation, poroelastic rebound, slow slip events, long-term creep, gravity-driven postseismic deformation).
Primary Convener:  Chris Rollins, California Institute of Technology, Pasadena, CA, United States
Conveners:  Adriano Gualandi, California Institute of Technology, Geological and Planetary Sciences, Pasadena, CA, United States, Mong-Han Huang, NASA Jet Propulsion Laboratory, Pasadena, CA, United States and Jessica R Murray, USGS Western Regional Offices Menlo Park, Menlo Park, United States
Chairs:  Adriano Gualandi, California Institute of Technology, Geological and Planetary Sciences, Pasadena, CA, United States, Chris Rollins, California Institute of Technology, Pasadena, CA, United States and Mong-Han Huang, University of Maryland College Park, College Park, MD, United States
OSPA Liaison:  Chris Rollins, California Institute of Technology, Pasadena, CA, United States

Cross-Listed:
  • T - Tectonophysics
Index Terms:

Abstracts Submitted to this Session:

Sharon Kedar1, Yehuda Bock2, Angelyn W Moore3, Peng Fang4, Zhen Liu5, Anne Sullivan2, Donald F Argus6, Songnian Jiang7 and Scott T Marshall8, (1)Jet Propulsion Laboratory, Pasadena, CA, United States, (2)Scripps Institution of Oceanography, University of California San Diego, Institute of Geophysics and Planetary Physics, La Jolla, United States, (3)Jet Propulsion Lab Caltech, Pasadena, United States, (4)Scripps Institution of Oceanography, Institute of Geophysics and Planetary Physics, La Jolla, CA, United States, (5)Jet Propulsion Laboratory, Pasadena, United States, (6)Jet Propulsion Laboratory, California Institute of Technology, Pasadena, United States, (7)Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, La Jolla, CA, United States, (8)Appalachian State University, Department of Geological and Environmental Sciences, Boone, NC, United States
Thora Arnadottir, University of Iceland, Nordic Volcanological Center, Institute of Earth Sciences, Reykjavik, Iceland, A. John Haines, GNS Science, Dunedin, New Zealand, Halldor Geirsson, University of Iceland, Faculty of Earth Sciences, Reykjavik, Iceland and Sigrun Hreinsdottir, GNS Science, Lower Hutt, New Zealand
Jonathan R. Bedford1, Michael G Bevis2, Juan Carlos Baez3, Marcos Moreno4, Zhiguo Deng4 and Christian Sippl1, (1)Deutsches GeoForschungsZentrum GFZ, Potsdam, Germany, (2)The Ohio State University, School of Earth Sciences, Columbus, United States, (3)Centro Sismologico National, Universidad de Chile, Santiago, Chile, (4)Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences, Potsdam, Germany
Cedric Twardzik, Géoazur - Université Nice Sophia Antipolis, Valbonne, France, Mathilde Vergnolle, CNRS, Paris Cedex 16, France, Antonio Avallone, Istituto Nazionale di Geofisica e Vulcanologia, Roma, Italy and Anthony Sladen, CNRS, Géoazur - Université Côte d’Azur, Valbonne, France
Baptiste Rousset1, Michel Campillo2, Cecile Lasserre3, William Benjamin Frank4, Nathalie Cotte3, Andrea Walpersdorf5, Anne Socquet6 and Vladimir Kostoglodov7, (1)University of California Berkeley, Earth and Planetary Sciences Department, Berkeley, CA, United States, (2)ISTerre Institute of Earth Sciences, CNRS, Université Grenoble Alpes, Saint Martin d'Hères, France, (3)ISTerre Institute of Earth Sciences, Saint Martin d'Hères, France, (4)Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, Cambridge, MA, United States, (5)Université Grenoble Alpes, Institut des Sciences de la Terre, Grenoble, France, (6)University Grenoble Alpes, ISTerre Institute of Earth Sciences, Grenoble, France, (7)Universidad Nacional Autonoma de Mexico, Mexico City, Mexico
Laura M Wallace1,2, Sigrun Hreinsdottir2, Ian J Hamling2, Elisabetta D'Anastasio3 and Noel M Jackson4, (1)GEOMAR Helmholtz Centre for Ocean Research Kiel, Kiel, Germany, (2)GNS Science, Lower Hutt, New Zealand, (3)GNS Science Te Pῡ Ao, Wellington, New Zealand, (4)University of Missouri, Geological Sciences, Columbia, MO, United States

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