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Deformation Structures From Splay and Décollement Faults in the Nankai Accretionary Prism, SW Japan(IODP NanTroSEIZE Expedition 316): Evidence for Slow and Rapid Slip in Fault Rocks

Geochemistry, geophysics, geosystems : G3, 2020-06, Vol.21 (6), p.n/a

2020

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Superplastic deformation of ice: Experimental observations

Journal of Geophysical Research, 2001-06, Vol.106 (B6), p.11017-11030

2001

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Constitutive relationships and physical basis of fault strength due to flash heating

Journal of Geophysical Research - Solid Earth, 2008-01, Vol.113 (B1), p.B01401-n/a

2008

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Constraints on the Physical Mechanism of Frictional Aging From Nanoindentation

Geophysical research letters, 2018-12, Vol.45 (24), p.13,306-13,311

2018

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Viscous flow features on the surface of Mars: Observations from high-resolution Mars Orbiter Camera (MOC) images

Journal of Geophysical Research - Planets, 2003-06, Vol.108 (E6), p.5057-n/a

2003

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The Rheological Behavior of CO2 Ice: Application to Glacial Flow on Mars

Geophysical research letters, 2020-11, Vol.47 (22), p.n/a

2020

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Rheological and Thermal Properties of Icy Materials

Space science reviews, 2010-06, Vol.153 (1-4), p.273-298

2010

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Nanoscale Roughness of Natural Fault Surfaces Controlled by Scale‐Dependent Yield Strength

Geophysical research letters, 2017-09, Vol.44 (18), p.9299-9307

2017

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Seismic slip propagation to the updip end of plate boundary subduction interface faults: Vitrinite reflectance geothermometry on Integrated Ocean Drilling Program NanTro SEIZE cores

Geology (Boulder), 2011-04, Vol.39 (4), p.395-398

2011

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Making EBSD on water ice routine

Journal of microscopy (Oxford), 2015-09, Vol.259 (3), p.237-256

2015

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Dynamic weakening of serpentinite gouges and bare surfaces at seismic slip rates

Journal of geophysical research. Solid earth, 2014-11, Vol.119 (11), p.8107-8131

2014

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Friction falls towards zero in quartz rock as slip velocity approaches seismic rates

Nature, 2004-01, Vol.427 (6973), p.436-439

2004

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Interactions between deformation and fluids in the frontal thrust region of the NanTroSEIZE transect offshore the Kii Peninsula, Japan: Results from IODP Expedition 316 Sites C0006 and C0007

Geochemistry, geophysics, geosystems : G3, 2009-12, Vol.10 (12), p.Q0AD01-n/a

2009

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Grain boundary sliding in fine-grained Ice I

Scripta materialia, 1997-11, Vol.37 (9), p.1399-1406

1997

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Geological evidence for solid-state convection in Europa's ice shell

Nature (London), 1998-01, Vol.391 (6665), p.365-368

1998

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Geological evidence for solid-state convection in Europa's ice shell

Nature (London), 1998-01, Vol.391 (6665), p.365-368

1998

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Reply to comment by P. Duval and M. Montagnat on “Superplastic deformation of ice: Experimental observations”

Journal of Geophysical Research - Solid Earth, 2002-11, Vol.107 (B11), p.ECV 17-1-ECV 17-5

2002

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The Rheological Behavior of CO 2 Ice: Application to Glacial Flow on Mars

Geophysical research letters, 2020-11, Vol.47 (22)

2020

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Nanoindentation creep of quartz, with implications for rate- and state-variable friction laws relevant to earthquake mechanics

Journal of materials research, 2004-01, Vol.19 (1), p.357-365

2004

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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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Progressive illitization in fault gouge caused by seismic slip propagation along a megasplay fault in the Nankai Trough

Geology (Boulder), 2011-11, Vol.39 (11), p.995-998

2011

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Temperature and strain controls on ice deformation mechanisms: insights from the microstructures of samples deformed to progressively higher strains at −10, −20 and −30 °C

The cryosphere, 2020-11, Vol.14 (11), p.3875-3905

2020

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Crystallographic preferred orientations of ice deformed in direct-shear experiments at low temperatures

The cryosphere, 2019-02, Vol.13 (1), p.351-371

2019

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Grain growth of natural and synthetic ice at 0 °C

The cryosphere, 2023-08, Vol.17 (8), p.3443-3459

2023

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Low frictional strength of quartz rocks at subseismic slip rates

Geophysical research letters, 2002-09, Vol.29 (17), p.25-1-25-4

2002

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Deformation Structures From Splay and Décollement Faults in the Nankai Accretionary Prism, SW Japan(IODP NanTroSEIZE Expedition 316): Evidence for Slow and Rapid Slip in Fault Rocks

Superplastic deformation of ice: Experimental observations

Constitutive relationships and physical basis of fault strength due to flash heating

Constraints on the Physical Mechanism of Frictional Aging From Nanoindentation

Viscous flow features on the surface of Mars: Observations from high-resolution Mars Orbiter Camera (MOC) images

The Rheological Behavior of CO2 Ice: Application to Glacial Flow on Mars

Rheological and Thermal Properties of Icy Materials

Nanoscale Roughness of Natural Fault Surfaces Controlled by Scale‐Dependent Yield Strength

Seismic slip propagation to the updip end of plate boundary subduction interface faults: Vitrinite reflectance geothermometry on Integrated Ocean Drilling Program NanTro SEIZE cores

Making EBSD on water ice routine

Dynamic weakening of serpentinite gouges and bare surfaces at seismic slip rates

Friction falls towards zero in quartz rock as slip velocity approaches seismic rates

Interactions between deformation and fluids in the frontal thrust region of the NanTroSEIZE transect offshore the Kii Peninsula, Japan: Results from IODP Expedition 316 Sites C0006 and C0007

Grain boundary sliding in fine-grained Ice I

Geological evidence for solid-state convection in Europa's ice shell

Geological evidence for solid-state convection in Europa's ice shell

Reply to comment by P. Duval and M. Montagnat on “Superplastic deformation of ice: Experimental observations”

The Rheological Behavior of CO 2 Ice: Application to Glacial Flow on Mars

Nanoindentation creep of quartz, with implications for rate- and state-variable friction laws relevant to earthquake mechanics

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

Progressive illitization in fault gouge caused by seismic slip propagation along a megasplay fault in the Nankai Trough

Temperature and strain controls on ice deformation mechanisms: insights from the microstructures of samples deformed to progressively higher strains at −10, −20 and −30 °C

Crystallographic preferred orientations of ice deformed in direct-shear experiments at low temperatures

Grain growth of natural and synthetic ice at 0 °C

Low frictional strength of quartz rocks at subseismic slip rates

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