- 10 Mar 2023
- 1:00 PM PST
- 2:00 PM PST
FM: Fault strength evolution during the seismic cycle: Insights from the laboratory
John Bedford, University of Liverpool Geophysical evidence suggests that some faults are frictionally strong, in agreement with laboratory measurements of quasi-static frictional strength (μ ≈ 0.6-0.8) for many crustal materials; whereas others studies have found that some faults...