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Pressure Solution Grain Boundary Sliding as a Large Strain Mechanism of Superplastic Flow in the Upper Crust

Journal of geophysical research. Solid earth, 2023-04, Vol.128 (4), p.n/a

2023

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The Role of Pressure Solution Creep in the Ductility of the Earth’s Upper Crust

Advances in Geophysics, 2013, Vol.54, p.47-179

2013

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Lithological control on the deformation mechanism and the mode of fault slip on the Longitudinal Valley Fault, Taiwan

Tectonophysics, 2014-09, Vol.632, p.48-63

2014

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A microstructural study of fault rocks from the SAFOD: Implications for the deformation mechanisms and strength of the creeping segment of the San Andreas Fault

Journal of structural geology, 2012-09, Vol.42, p.246-260

2012

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Compaction and Porosity Reduction in Carbonates: A Review of Observations, Theory, and Experiments

Advances in Geophysics, 2013, Vol.54, p.181-238

2013

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200-m-deep earthquake swarm in Tricastin (lower Rhône Valley, France) accounts for noisy seismicity over past centuries

Terra nova (Oxford, England), 2009-06, Vol.21 (3), p.203-210

2009

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Rock and mineral transformations in a fault zone leading to permanent creep: Interactions between brittle and viscous mechanisms in the San Andreas Fault

Journal of geophysical research. Solid earth, 2014-11, Vol.119 (11), p.8132-8153

2014

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Kinetics of crack-sealing, intergranular pressure solution, and compaction around active faults

Journal of structural geology, 2000-10, Vol.22 (10), p.1395-1407

2000

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Intense fracturing and fracture sealing induced by mineral growth in porous rocks

Chemical geology, 2010-01, Vol.269 (3), p.197-209

2010

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Evolution of fault permeability during episodic fluid circulation: Evidence for the effects of fluid–rock interactions from travertine studies (Utah–USA)

Tectonophysics, 2015-05, Vol.651-652 (651), p.121-137

2015

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Geochemical transect through a travertine mount: A detailed record of CO2-enriched fluid leakage from Late Pleistocene to present-day – Little Grand Wash fault (Utah, USA)

Quaternary international, 2017-05, Vol.437, p.98-106

2017

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Strength evolution of a reactive frictional interface is controlled by the dynamics of contacts and chemical effects

Earth and planetary science letters, 2012-08, Vol.341-344, p.20-34

2012

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Dating deep? Luminescence studies of fault gouge from the San Andreas Fault zone 2.6 km beneath Earth's surface

Quaternary geochronology, 2012-07, Vol.10, p.280-284

2012

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Pressure solution in sandstones: influence of clays and dependence on temperature and stress

Tectonophysics, 1997-10, Vol.280 (3), p.257-266

1997

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Carbon–oxygen isotope and trace element constraints on how fluids percolate faulted limestones from the San Andreas Fault system: partitioning of fluid sources and pathways

Chemical geology, 2002-10, Vol.190 (1), p.231-250

2002

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Quantifying the Partition Between Seismic and Aseismic Deformation Along Creeping and Locked Sections of the North Anatolian Fault, Turkey

Pure and applied geophysics, 2019-03, Vol.176 (3), p.1293-1321

2019

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Microstructures Induced in Porous Limestone by Dynamic Loading, and Fracture Healing: An Experimental Approach

Pure and applied geophysics, 2015-05, Vol.172 (5), p.1269-1290

2015

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Reply to the comment on “First records of syn-diagenetic non-tectonic folding in Quaternary thermogene travertines caused by hydrothermal incremental veining” by Billi et alii

Tectonophysics, 2017-11, Vol.721, p.501-512

2017

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Dynamics of a dissolution front for solids under stress

Geophysical research letters, 2004-03, Vol.31 (6), p.L06618-n/a

2004

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First records of syn-diagenetic non-tectonic folding in quaternary thermogene travertines caused by hydrothermal incremental veining

Tectonophysics, 2017-03, Vol.700-701, p.60-79

2017

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Kinematic models of deformation at the front of the Alps: new data from map-view restoration

Swiss Journal of geosciences, 2008, Vol.101 (2), p.289-303

2008

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Evidence of transient increases of fluid pressure in SAFOD phase III cores

Geophysical research letters, 2011-02, Vol.38 (3), p.np-n/a

2011

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Variety of stylolites' morphologies and statistical characterization of the amount of heterogeneities in the rock

Journal of structural geology, 2007-01, Vol.29 (3), p.422-434

2007

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Fluid pressure evolution during the earthquake cycle controlled by fluid flow and pressure solution crack sealing

Earth, planets, and space, 2002-01, Vol.54 (11), p.1139-1146

2002

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How pressure solution creep and fracturing processes interact in the upper crust to make it behave in both a brittle and viscous manner

Journal of structural geology, 1999-08, Vol.21 (8), p.1189-1197

1999

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Pressure Solution Grain Boundary Sliding as a Large Strain Mechanism of Superplastic Flow in the Upper Crust

The Role of Pressure Solution Creep in the Ductility of the Earth’s Upper Crust

Lithological control on the deformation mechanism and the mode of fault slip on the Longitudinal Valley Fault, Taiwan

A microstructural study of fault rocks from the SAFOD: Implications for the deformation mechanisms and strength of the creeping segment of the San Andreas Fault

Compaction and Porosity Reduction in Carbonates: A Review of Observations, Theory, and Experiments

200-m-deep earthquake swarm in Tricastin (lower Rhône Valley, France) accounts for noisy seismicity over past centuries

Rock and mineral transformations in a fault zone leading to permanent creep: Interactions between brittle and viscous mechanisms in the San Andreas Fault

Kinetics of crack-sealing, intergranular pressure solution, and compaction around active faults

Intense fracturing and fracture sealing induced by mineral growth in porous rocks

Evolution of fault permeability during episodic fluid circulation: Evidence for the effects of fluid–rock interactions from travertine studies (Utah–USA)

Geochemical transect through a travertine mount: A detailed record of CO2-enriched fluid leakage from Late Pleistocene to present-day – Little Grand Wash fault (Utah, USA)

Strength evolution of a reactive frictional interface is controlled by the dynamics of contacts and chemical effects

Dating deep? Luminescence studies of fault gouge from the San Andreas Fault zone 2.6 km beneath Earth's surface

Pressure solution in sandstones: influence of clays and dependence on temperature and stress

Carbon–oxygen isotope and trace element constraints on how fluids percolate faulted limestones from the San Andreas Fault system: partitioning of fluid sources and pathways

Quantifying the Partition Between Seismic and Aseismic Deformation Along Creeping and Locked Sections of the North Anatolian Fault, Turkey

Microstructures Induced in Porous Limestone by Dynamic Loading, and Fracture Healing: An Experimental Approach

Reply to the comment on “First records of syn-diagenetic non-tectonic folding in Quaternary thermogene travertines caused by hydrothermal incremental veining” by Billi et alii

Dynamics of a dissolution front for solids under stress

First records of syn-diagenetic non-tectonic folding in quaternary thermogene travertines caused by hydrothermal incremental veining

Kinematic models of deformation at the front of the Alps: new data from map-view restoration

Evidence of transient increases of fluid pressure in SAFOD phase III cores

Variety of stylolites' morphologies and statistical characterization of the amount of heterogeneities in the rock

Fluid pressure evolution during the earthquake cycle controlled by fluid flow and pressure solution crack sealing

How pressure solution creep and fracturing processes interact in the upper crust to make it behave in both a brittle and viscous manner

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