Seismic and aseismic slip indicators in serpentinite gouge

Geology

Volumn 28, Issue 2, 2000, Pages 135-138

  Reinen, L A ^a  

^a POMONA COLLEGE   (United States)

Author keywords

Creep; Earthquake; Fault; Microstructures; Serpentine; Serpentinite

Indexed keywords

CREEP; EARTHQUAKES; FAULTING; MAGNESITE; MICROSTRUCTURE; SERPENTINE; SILICATE MINERALS; STRUCTURAL GEOLOGY;

ASEISMIC FAULTS; CRYSTALLOGRAPHIC PREFERRED ORIENTATIONS; DISTRIBUTED DEFORMATION; FRICTION EXPERIMENTS; LOCALIZED DEFORMATIONS; SEISMIC BEHAVIOR; SEISMIC SLIPS; SERPENTINITE;

FAULT SLIPS;

FAULT; FAULT GOUGE; FAULT SLIP; SERPENTINE; SERPENTINITE;

CALIFORNIA; MONTEREY COUNTY; UNITED STATES;

EID: 84874995995     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(2000)028<0135:SAASII>2.3.CO;2     Document Type: Article

References (16)

1. Composite planar fabric of gouge from the Punchbowl fault, California
2. Direct observations of frictional contacts: New insights for state-dependent properties
3. Nondilatant brittle deformation of serpentinites: Implications for Mohr-Coulomb theory and the strength of faults
4. Structures in natural serpentinite gouges
5. Microstructures in natural serpentinite gouges
6. Strength of chrysotile-serpentinite gouge under hydrothermal conditions: Can it explain a weak San Andreas fault?
7. Strengths of serpentinite gouges at elevated temperatures
8. Microstructure of serpentinite mylonites from the Josephine ophiolite and serpentinization in retrogressive shear zones, California
9. Strain variations in shear belts
10. Microstructural evidence of strain localization and distributed strain in serpentine friction experiments
11. The frictional behavior of serpentinite: Implications for aseismic creep on shallow crustal faults
12. The frictional behavior of lizardite and antigorite serpentinites: Experiments, constitutive models, and implications for natural faults
13. Stability of steady frictional slipping
14. Rock friction constitutive behavior from laboratory experiments and its implications for an earthquake prediction field monitoring program
15. The effect of pore fluid chemistry on the frictional evolution effect