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Nature, ISSN 0028-0836, 2009, Volume 462, Issue 7275, pp. 907 - 910
Geological and geophysical evidence suggests that some crustal faults are weak1–6 compared to laboratory measurements of frictional strength7. Explanations for... 
SYSTEM | FRICTIONAL BEHAVIOR | CORES | SAN-ANDREAS FAULT | SLIP | GOUGE | ROCKS | MULTIDISCIPLINARY SCIENCES | STRENGTH | STRESS | CLAY | Faults (Geology) | Rocks | Research | Varieties | Grain size | Earthquakes | Seismology | Shear stresses | Mass spectrometry | Velocity | Strain hardening
Journal Article
Earth-Science Reviews, ISSN 0012-8252, 12/2013, Volume 127, pp. 171 - 192
Journal Article
Geophysical Research Letters, ISSN 0094-8276, 09/2018, Volume 45, Issue 17, pp. 8976 - 8984
Journal Article
Geochemistry, Geophysics, Geosystems, ISSN 1525-2027, 05/2016, Volume 17, Issue 5, pp. 1778 - 1798
The main San Andreas Fault strikes subparallel to compressional folds and thrust faults. Its fault‐normal traction is on average a factor of γ = 1 + 2 μ thr (... 
San Andreas Fault | nonlinear seismic waves | heat flow paradox | rupture tip | GROUND-MOTION SIMULATIONS | SAFOD PILOT HOLE | STRIKE-SLIP | STRESS MEASUREMENTS | GEOCHEMISTRY & GEOPHYSICS | SHEAR VELOCITY ANISOTROPY | INTRAPLATE LITHOSPHERE | EARTHQUAKE RUPTURES | LOS-ANGELES BASIN | SOUTHERN CALIFORNIA | RATE-WEAKENING FRICTION | Seismology | Plate tectonics | Fault lines
Journal Article