- G13A: Subduction Zone Deformation Throughout the Earthquake Cycle: Observations and Models I Oral
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NOLA CC
Primary Convener:Generic 'disconnected' Message
Kaj Johnson, Indiana University Bloomington
Convener:
Kelin Wang, Pacific Geoscience Centre, Geological Survey of Canada
Camilla Cattania, Deutsches GeoForschungsZentrum GFZ
Early Career Convener:
Nicolás Castro Perdomo, Indiana University Bloomington
Chair:
Kaj Johnson, Indiana University
Nicolás Castro Perdomo, Indiana University Bloomington
Subduction zones are the source of Earth's largest earthquakes, posing significant hazards to densely populated coastal regions. Recent advances in space geodesy have greatly improved our ability to monitor complex deformation processes throughout the earthquake cycle. We invite contributions investigating the full spectrum of subduction zone processes, including interseismic coupling, coseismic slip, slow slip events, fault creep, episodic tremor and slip (ETS), postseismic afterslip, and viscoelastic mantle flow transients. We particularly encourage studies that integrate space geodetic data (e.g., GNSS, InSAR) with seismic, paleoseismic, and geological observations, as well as numerical modeling to illuminate the physical mechanisms driving these processes, their spatial distribution and temporal evolution.
Index Terms
1207 Transient deformation
1242 Seismic cycle related deformations
7240 Subduction zones
8170 Subduction zone processes
Cross-Listed:
T - Tectonophysics
S - Seismology
Neighborhoods:
2. Earth Interior
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