T13D:
Whose Fault Is It? Relating Structural and Compositional Heterogeneity to Slip Behavior II Posters
T13D:
Whose Fault Is It? Relating Structural and Compositional Heterogeneity to Slip Behavior II Posters
Whose Fault Is It? Relating Structural and Compositional Heterogeneity to Slip Behavior II Posters
Submit an Abstract to this Session
Session ID#: 49102
Session Description:
Large plate boundary fault systems are commonly rheologically segmented both along strike and down dip, including across the transition from seismic to aseismic shear displacement. In addition to thermal controls, these variations in slip style may arise due to geometric or compositional heterogeneities along the fault zone. Many questions remain on the relationships between structure and fault behavior. For example, how does rupture propagation interact with roughness or material properties along a fault at a range of slip rates? How does this impact the global variability in seismic behavior at plate boundaries? In this session, we will highlight recent advances in characterizing observed structures, geophysical properties, lithologies, and slip behaviors at plate boundary faults at a range of scales, with a focus on relationships between these features. We encourage submissions from seismology, magnetotellurics, geodesy, earthquake rupture modeling, structural geology, fault zone drilling, and experimental work.
Primary Convener: Hannah S Rabinowitz, Brown University, Providence, RI, United States
Conveners: Helen A Janiszewski, Carnegie Institution for Science, Department of Terrestrial Magnetism, Washington, DC, United States, Ake Fagereng, Cardiff University, Cardiff, CF24, United Kingdom and Samer Naif, Lamont -Doherty Earth Observatory, Palisades, NY, United States
Primary Liaison: Hannah S Rabinowitz, Brown University, Providence, RI, United States
Chairs: Hannah S Rabinowitz, Columbia University in the City of New York, New York, NY, United States, Helen A Janiszewski, University of Hawaii at Manoa, Department of Earth Sciences, Honolulu, HI, United States and Ake Fagereng, Cardiff University, Department of Earth and Environmental Sciences, Cardiff, United Kingdom
OSPA Liaison: Samer Naif, Scripps Institution of Oceanography, La Jolla, United States
Co-Organized
with:
Tectonophysics, SPA-Magnetospheric Physics, Mineral and Rock Physics, and Seismology
Tectonophysics, SPA-Magnetospheric Physics, Mineral and Rock Physics, and Seismology
Proposed Co-Organized Session with:
- MR - Mineral and Rock Physics
- S - Seismology
- SM - SPA-Magnetospheric Physics
Index Terms:
1209 Tectonic deformation [GEODESY AND GRAVITY]
7230 Seismicity and tectonics [SEISMOLOGY]
8118 Dynamics and mechanics of faulting [TECTONOPHYSICS]
8163 Rheology and friction of fault zones [TECTONOPHYSICS]
Abstracts Submitted to this Session:
Serpentinite slickenfibres: analogues for small repeating earthquakes at the slab-mantle interface? (426929)
See more of: Tectonophysics
