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Disclinations and disconnections in minerals and metals

Proceedings of the National Academy of Sciences - PNAS, 2020-01, Vol.117 (1), p.196-204

2020

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Reaction-driven cracking during retrograde metamorphism: Olivine hydration and carbonation

Earth and planetary science letters, 2012-09, Vol.345-348, p.81-89

2012

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Role of pore fluid pressure on transient strength changes and fabric development during serpentine dehydration at mantle conditions: Implications for subduction-zone seismicity

Earth and planetary science letters, 2015-07, Vol.421, p.1-12

2015

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Elastic Impact Consequences for High‐Frequency Earthquake Ground Motion

Geophysical research letters, 2020-03, Vol.47 (5), p.n/a

2020

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Plagioclase preferred orientation in layered mylonites: Evaluation of flow laws for the lower crust

Journal of Geophysical Research - Solid Earth, 2008-05, Vol.113 (B5), p.B05202-n/a

2008

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Fault Interactions Enhance High‐Frequency Earthquake Radiation

Geophysical research letters, 2021-10, Vol.48 (20), p.n/a

2021

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Microstructural evidence for the transition from dislocation creep to dislocation-accommodated grain boundary sliding in naturally deformed plagioclase

Journal of structural geology, 2016-11, Vol.92, p.30-45

2016

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Rheological properties of the mantle lid beneath the Mojave region in southern California

Earth and planetary science letters, 2014-05, Vol.393, p.60-72

2014

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High‐Frequency Ground Motions of Earthquakes Correlate With Fault Network Complexity

Geophysical research letters, 2024-06, Vol.51 (12), p.n/a

2024

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High-resolution seismic constraints on flow dynamics in the oceanic asthenosphere

Nature (London), 2016-07, Vol.535 (7613), p.538-541

2016

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Rheologic controls on slab dynamics

Geochemistry, geophysics, geosystems : G3, 2007-08, Vol.8 (8), p.Q08012-n/a

2007

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Ductile deformation during carbonation of serpentinized peridotite

Nature communications, 2022-06, Vol.13 (1), p.3478-3478, Article 3478

2022

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Using short-term postseismic displacements to infer the ambient deformation conditions of the upper mantle

Journal of Geophysical Research: Solid Earth, 2012-01, Vol.117 (B1), p.n/a

2012

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Olivine friction at the base of oceanic seismogenic zones

Journal of Geophysical Research - Solid Earth, 2007-01, Vol.112 (B1), p.B01205-n/a

2007

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Evolution of olivine lattice preferred orientation during simple shear in the mantle

Earth and planetary science letters, 2008-08, Vol.272 (3), p.501-512

2008

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Plastic anisotropy and fabric evolution in sheared and recrystallized quartz single crystals

Journal of Geophysical Research, 2011-02, Vol.116 (B2), p.n/a, Article B02206

2011

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The role of grain size evolution in the rheology of ice: implications for reconciling laboratory creep data and the Glen flow law

The cryosphere, 2021-09, Vol.15 (9), p.4589-4605

2021

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Rheology of the Upper Mantle and the Mantle Wedge: A View from the Experimentalists

Inside the Subduction Factory, 2004-01, p.83-105

2004

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Thermal-mechanical behavior of oceanic transform faults: Implications for the spatial distribution of seismicity

Geochemistry, geophysics, geosystems : G3, 2010-07, Vol.11 (7), p.np-n/a

2010

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Water in the oceanic upper mantle: implications for rheology, melt extraction and the evolution of the lithosphere

Earth and planetary science letters, 1996-10, Vol.144 (1), p.93-108

1996

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Flash weakening of serpentinite at near-seismic slip rates

Journal of Geophysical Research, 2011-03, Vol.116 (B3), p.n/a, Article B03202

2011

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The electrical structure of the central Pacific upper mantle constrained by the NoMelt experiment

Geochemistry, geophysics, geosystems : G3, 2015-04, Vol.16 (4), p.1115-1132

2015

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Microstructural Shift due to Post‐Deformation Annealing in the Upper Mantle

Geochemistry, geophysics, geosystems : G3, 2021-03, Vol.22 (3), p.n/a

2021

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Geophysical evidence from the MELT area for compositional controls on oceanic plates

Nature, 2005-09, Vol.437 (7056), p.249-252

2005

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Deformation mechanisms of antigorite serpentinite at subduction zone conditions determined from experimentally and naturally deformed rocks

Earth and planetary science letters, 2015-02, Vol.411, p.229-240

2015

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Disclinations and disconnections in minerals and metals

Reaction-driven cracking during retrograde metamorphism: Olivine hydration and carbonation

Role of pore fluid pressure on transient strength changes and fabric development during serpentine dehydration at mantle conditions: Implications for subduction-zone seismicity

Elastic Impact Consequences for High‐Frequency Earthquake Ground Motion

Plagioclase preferred orientation in layered mylonites: Evaluation of flow laws for the lower crust

Fault Interactions Enhance High‐Frequency Earthquake Radiation

Microstructural evidence for the transition from dislocation creep to dislocation-accommodated grain boundary sliding in naturally deformed plagioclase

Rheological properties of the mantle lid beneath the Mojave region in southern California

High‐Frequency Ground Motions of Earthquakes Correlate With Fault Network Complexity

High-resolution seismic constraints on flow dynamics in the oceanic asthenosphere

Rheologic controls on slab dynamics

Ductile deformation during carbonation of serpentinized peridotite

Using short-term postseismic displacements to infer the ambient deformation conditions of the upper mantle

Olivine friction at the base of oceanic seismogenic zones

Evolution of olivine lattice preferred orientation during simple shear in the mantle

Plastic anisotropy and fabric evolution in sheared and recrystallized quartz single crystals

The role of grain size evolution in the rheology of ice: implications for reconciling laboratory creep data and the Glen flow law

Rheology of the Upper Mantle and the Mantle Wedge: A View from the Experimentalists

Thermal-mechanical behavior of oceanic transform faults: Implications for the spatial distribution of seismicity

Water in the oceanic upper mantle: implications for rheology, melt extraction and the evolution of the lithosphere

Flash weakening of serpentinite at near-seismic slip rates

The electrical structure of the central Pacific upper mantle constrained by the NoMelt experiment

Microstructural Shift due to Post‐Deformation Annealing in the Upper Mantle

Geophysical evidence from the MELT area for compositional controls on oceanic plates

Deformation mechanisms of antigorite serpentinite at subduction zone conditions determined from experimentally and naturally deformed rocks

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