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Generation and maintenance of pore pressure excess in a dehydrating system 2. Theoretical analysis
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What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
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Mechanistic interactions between deformation and metamorphism
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Fluid Flow during Metamorphism and its Implications for Fluid—Rock Ratios
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The Permeation of Water into Hydrating Shear Zones
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Fluid and enthalpy production during regional metamorphism
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Laboratory measurement of compaction-induced permeability change in porous rocks: Implications for the generation and maintenance of pore pressure excess in the crust
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The role of fluids in crustal processes
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Conduction of heat in solids
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The effect of decomposition of hydrous minerals on the mechanical properties of rocks at high pressures and temperatures
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Some geophysical implications of the deformation and metamorphism of the Ivrea zone, northern Italy
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Deformation and pore pressure in dehydrating gypsum under transiently drained conditions
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Permeability of crystalline and argillaceous rocks
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Fluid flow and transport in rocks; mechanisms and effects
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Chapter 20 Fault Stress States, Pore Pressure Distributions, and the Weakness of the San Andreas Fault
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Crustal‐scale fluid transport: Magnitude and mechanisms
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A historical review of metamorphic fluid flow
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The transition from weakening to strengthening in dehydrating gypsum: Evolution of excess pore pressures
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Network modeling of permeability evolution during cementation and hot isostatic pressing
inferredcites →https://doi.org/10.1029/96jb02485openalex-snapshot
Generation and maintenance of pore pressure excess in a dehydrating system 1. Experimental and microstructural observations
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Introduction to Groundwater Modeling: Finite Difference and Finite Element Methods
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Limits on lithospheric stress imposed by laboratory experiments
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Porosity reduction and crustal pore pressure development
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Experimental deformation of serpentinite and its tectonic implications
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Tectonic Implications of Gypsum Dehydration
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On the Maintenance of Anomalous Fluid Pressures: I. Thick Sedimentary Sequences
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On the Maintenance of Anomalous Fluid Pressures: II. Source Layer at Depth
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The hydrodynamics of contact metamorphism
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Kinetics of hydrofracturing and metamorphic veining
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The generation and dissipation of abnormal fluid pressures in active depositional environments
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Transformation- and reaction-enhanced ductility in rocks
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Finite Difference Methods in Heat Transfer
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The Role of Fluids in Crustal Processes
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Dehydration-induced pore-fluid pressure anomalies and the weakening of rocks
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7. Instability of Deformation
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inferred← citeshttps://doi.org/10.70675/f2cf25a9zda56z4a64z8fb2z3ef253ccffd1openalex-snapshot
Reproduction expérimentale d'analogues de séismes mantelliques par déshydratation de l'antigorite & Comparaison à des pseudotachylites naturelles
inferred← citeshttps://doi.org/10.7301/z0kw5ddjopenalex-snapshot
Dynamics of Melt-Lithosphere Interaction
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