T42D:
The Nature of Creeping Faults: Where, Why, and How They Slip Slowly I
T42D:
The Nature of Creeping Faults: Where, Why, and How They Slip Slowly I
The Nature of Creeping Faults: Where, Why, and How They Slip Slowly I
Submit an Abstract to this Session
Session ID#: 59409
Session Description:
Fault creep has been observed worldwide in continental regions as well as on many subduction thrusts. With improved resolution of fault kinematics using dense geodetic and seismologic data, the spatial distribution of fault creep has been intensively investigated on a variety of faults. In rock mechanics experiments, the frictional behavior of fault materials has been studied to better understand what enables a fault to creep. How much do we know about the similarities and differences between shallow creep (upper few km) and deep creep (>10 km deep) from microstructures, mineral composition, lithologic properties and conditions, geodesy, and geophysical methods? How well can we define zones of aseismic slip through integrated data? The goal of this session is to bring together different disciplines for improving our understanding on why and how faults creep. We encourage multi-disciplinary contributions from geological, geophysical, experimental, and modeling studies of creeping faults.
Primary Convener: Kate Huihsuan Chen, National Taiwan Normal University, Department of Earth Sciences, Taipei, Taiwan
Convener: Roland Burgmann, University of California Berkeley, Earth and Planetary Science, Berkeley, United States
Primary Liaison: Kate Huihsuan Chen, Department of Earth Sciences, National Taiwan Normal University, Taipei, Taiwan
Chairs: Kate Huihsuan Chen, Department of Earth Sciences, National Taiwan Normal University, Taipei, Taiwan and Roland Burgmann, University of California Berkeley, Earth and Planetary Science, Berkeley, United States
OSPA Liaison: Kate Huihsuan Chen, Department of Earth Sciences, National Taiwan Normal University, Taipei, Taiwan
Cross-Listed:
- G - Geodesy
- MR - Mineral and Rock Physics
- NS - Near Surface Geophysics
- S - Seismology
Index Terms:
5112 Microstructure [PHYSICAL PROPERTIES OF ROCKS]
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:
A long-term view of Cascadia ETS (439527)
Shallow Fault Slip and Near-fault Deformation on the Creeping Section of the San Andreas Fault (409193)
The Mechanics of Slow Slip (Invited) (405657)
See more of: Tectonophysics
