T002
Characteristics of faults and fault zones and their influence on earthquake physics: observations, models, and experiments
Characteristics of faults and fault zones and their influence on earthquake physics: observations, models, and experiments
Session ID#: 248094
Session Description:
Fault zone structures in the upper crust are characterized by highly localized slip surfaces surrounded by intensely fractured rock. These slip surfaces are often geometrically complex and topographically rough over many orders of magnitude. The damage zone surrounding the slip surface has variability in size, shape, and fracture density that alters the permeability and rheology of the volume. Studies show that quantifiable parameters of faults and fault zones influence fundamental properties of earthquakes including the nucleation, propagation, slip distribution, strain energy budget, and ground motion. However, more work is necessary to improve our understanding of the relationship between earthquakes and the structures that host them. In this session, we welcome contributions from a variety of disciplines to better understand the manifestation and evolution of faults and fault zones in nature as well as the impact of structural variability on the behavior of earthquakes.
Co-Sponsor(s):
- MR - Mineral and Rock Physics
- S - Seismology
Index Terms:
7209 Earthquake dynamics [SEISMOLOGY]
8118 Dynamics and mechanics of faulting [TECTONOPHYSICS]
8123 Dynamics: seismotectonics [TECTONOPHYSICS]
8163 Rheology and friction of fault zones [TECTONOPHYSICS]
Primary Convener: James Atterholt, United States Geological Survey, Golden, United States
Conveners: Travis Alongi, USGS Earthquake Science Center, Moffett Field, United States, Yihe Huang, Earth and Environmental Sciences Department, University of Michigan, Ann Arbor, United States and Monica R Barbery, Brown University, Department of Earth, Environmental and Planetary Sciences, Providence, United States
See more of: Tectonophysics