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Direct Evidence for Fluid Pressure, Dilatancy, and Compaction Affecting Slip in Isolated Faults

Geophysical research letters, 2020-08, Vol.47 (16), p.n/a

2020

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Rapid Acceleration Leads to Rapid Weakening in Earthquake-Like Laboratory Experiments

Science (American Association for the Advancement of Science), 2012-10, Vol.338 (6103), p.101-105

2012

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Pseudotachylyte increases the post-slip strength of faults

Geology (Boulder), 2016-12, Vol.44 (12), p.1003-1006

2016

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Time‐Dependent Weakening of Granite at Hydrothermal Conditions

Geophysical research letters, 2023-11, Vol.50 (21), p.n/a

2023

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Evolution of fracture permeability of ultramafic rocks undergoing serpentinization at hydrothermal conditions: An experimental study

Geochemistry, geophysics, geosystems : G3, 2016-01, Vol.17 (1), p.44-55

2016

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Premonitory acoustic emissions and stick-slip in natural and smooth-faulted Westerly granite

Journal of Geophysical Research - Solid Earth, 2009-02, Vol.114 (B2), p.B02205-n/a

2009

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Frictional strength of wet and dry montmorillonite

Journal of geophysical research. Solid earth, 2017-05, Vol.122 (5), p.3392-3409

2017

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Why earthquakes correlate weakly with the solid Earth tides: Effects of periodic stress on the rate and probability of earthquake occurrence

Journal of Geophysical Research - Solid Earth, 2003-08, Vol.108 (B8), p.2391-n/a

2003

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Evolution of Wear and Friction Along Experimental Faults

Pure and applied geophysics, 2014-11, Vol.171 (11), p.3125-3141

2014

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Laboratory triggering of stick-slip events by oscillatory loading in the presence of pore fluid with implications for physics of tectonic tremor

Journal of Geophysical Research: Solid Earth, 2012-11, Vol.117 (B11), p.n/a

2012

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The effect of mineral bond strength and adsorbed water on fault gouge frictional strength

Geophysical research letters, 2000-03, Vol.27 (6), p.815-818

2000

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Permeability reduction in granite under hydrothermal conditions

Journal of Geophysical Research: Solid Earth, 2001-12, Vol.106 (B12), p.30551-30560

2001

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Pore fluid pressure, apparent friction, and Coulomb failure

Journal of Geophysical Research, 2000-11, Vol.105 (B11), p.25533-25542

2000

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The susceptibility of Oklahoma’s basement to seismic reactivation

Nature geoscience, 2019-10, Vol.12 (10), p.839-844

2019

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Quantitative measure of the variation in fault rheology due to fluid-rock interactions

Journal of Geophysical Research: Solid Earth, 1998-05, Vol.103 (B5), p.9691-9712

1998

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Earthquake Rupture at Focal Depth, Part II: Mechanics of the 2004 M2.2 Earthquake Along the Pretorius Fault, TauTona Mine, South Africa

Pure and applied geophysics, 2011-12, Vol.168 (12), p.2427-2449

2011

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Quasi-static fault growth and shear fracture energy in granite

Nature (London), 1991-03, Vol.350 (6313), p.39-42

1991

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Nucleation and growth of faults in brittle rocks

Journal of Geophysical Research - Solid Earth, 1994-09, Vol.99 (B9), p.18159-18173

1994

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Low resistivity and permeability in actively deforming shear zones on the San Andreas Fault at SAFOD

Journal of geophysical research. Solid earth, 2015-12, Vol.120 (12), p.8240-8258

2015

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Strengths of serpentinite gouges at elevated temperatures

Journal of Geophysical Research: Solid Earth, 1997-07, Vol.102 (B7), p.14787-14801

1997

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Frictional slip of granite at hydrothermal conditions

Journal of Geophysical Research: Solid Earth, 1995-07, Vol.100 (B7), p.13045-13064

1995

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Conversion of Wet Glass to Melt at Lower Seismogenic Zone Conditions: Implications for Pseudotachylyte Creep

Geophysical research letters, 2017-10, Vol.44 (20), p.10,248-10,255

2017

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Crystallographic controls on the frictional behavior of dry and water-saturated sheet structure minerals

Journal of Geophysical Research - Solid Earth, 2004-03, Vol.109 (B3), p.B03401-n/a

2004

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A Geology and Geodesy Based Model of Dynamic Earthquake Rupture on the Rodgers Creek‐Hayward‐Calaveras Fault System, California

Journal of geophysical research. Solid earth, 2021-03, Vol.126 (3), p.n/a

2021

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Deep permeability of the San Andreas Fault from San Andreas Fault Observatory at Depth (SAFOD) core samples

Journal of structural geology, 2014-07, Vol.64, p.99-114

2014

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Direct Evidence for Fluid Pressure, Dilatancy, and Compaction Affecting Slip in Isolated Faults

Rapid Acceleration Leads to Rapid Weakening in Earthquake-Like Laboratory Experiments

Pseudotachylyte increases the post-slip strength of faults

Time‐Dependent Weakening of Granite at Hydrothermal Conditions

Evolution of fracture permeability of ultramafic rocks undergoing serpentinization at hydrothermal conditions: An experimental study

Premonitory acoustic emissions and stick-slip in natural and smooth-faulted Westerly granite

Frictional strength of wet and dry montmorillonite

Why earthquakes correlate weakly with the solid Earth tides: Effects of periodic stress on the rate and probability of earthquake occurrence

Evolution of Wear and Friction Along Experimental Faults

Laboratory triggering of stick-slip events by oscillatory loading in the presence of pore fluid with implications for physics of tectonic tremor

The effect of mineral bond strength and adsorbed water on fault gouge frictional strength

Permeability reduction in granite under hydrothermal conditions

Pore fluid pressure, apparent friction, and Coulomb failure

The susceptibility of Oklahoma’s basement to seismic reactivation

Quantitative measure of the variation in fault rheology due to fluid-rock interactions

Earthquake Rupture at Focal Depth, Part II: Mechanics of the 2004 M2.2 Earthquake Along the Pretorius Fault, TauTona Mine, South Africa

Quasi-static fault growth and shear fracture energy in granite

Nucleation and growth of faults in brittle rocks

Low resistivity and permeability in actively deforming shear zones on the San Andreas Fault at SAFOD

Strengths of serpentinite gouges at elevated temperatures

Frictional slip of granite at hydrothermal conditions

Conversion of Wet Glass to Melt at Lower Seismogenic Zone Conditions: Implications for Pseudotachylyte Creep

Crystallographic controls on the frictional behavior of dry and water-saturated sheet structure minerals

A Geology and Geodesy Based Model of Dynamic Earthquake Rupture on the Rodgers Creek‐Hayward‐Calaveras Fault System, California

Deep permeability of the San Andreas Fault from San Andreas Fault Observatory at Depth (SAFOD) core samples

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