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Generation and maintenance of pore pressure excess in a dehydrating system 1. Experimental and microstructural observations
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What this work says
Outgoing claims: the papers this work cites, builds on, or argues with.
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Fluid Flow during Metamorphism and its Implications for Fluid—Rock Ratios
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On the Relationship between Deformation and Metamorphism, with Special Reference to the Behavior of Basic Rocks
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The Permeation of Water into Hydrating Shear Zones
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Thermodynamics of rock deformation by pressure solution
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Evolution of pore microstructures during healing of grain boundaries in synthetic calcite rocks
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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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Thermal dehydration reactions characterised by combined measurements of electrical conductivity and elastic wave velocities
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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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Chapter 20 Fault Stress States, Pore Pressure Distributions, and the Weakness of the San Andreas Fault
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Chapter 2 The Geology of Abnormal Pore Pressures
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Studies in Abnormal Pressures
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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
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Generation and maintenance of pore pressure excess in a dehydrating system 2. Theoretical analysis
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Experimental “sytectonic” dehydration of serpentinite under conditions of controlled pore water pressure
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Introduction to Special Section on the Role of Fluids in Sediment Accretion, Deformation, Diagenesis, and Metamorphism in Subduction Zones
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Evidence for a weak and overpressured décollement beneath sediment‐dominated accretionary prisms
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Experimental deformation of serpentinite and its tectonic implications
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The role of the fluid phase during regional metamorphism and deformation
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New Evidence on the State of Stress of the San Andreas Fault System
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Imaging the Pore Structure of Geomaterials
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ROLE OF FLUID PRESSURE IN MECHANICS OF OVERTHRUST FAULTING
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ROLE OF FLUID PRESSURE IN MECHANICS OF OVERTHRUST FAULTING
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ROLE OF FLUID PRESSURE IN MECHANICS OF OVERTHRUST FAULTING: REPLY
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Tectonic Implications of Gypsum Dehydration
inferredcites →https://doi.org/10.1130/0016-7606(1968)79[1097:otmoaf]2.0.co;2openalex-snapshot
On the Maintenance of Anomalous Fluid Pressures: I. Thick Sedimentary Sequences
inferredcites →https://doi.org/10.1130/0016-7606(1995)107<0595:thocm>2.3.co;2openalex-snapshot
The hydrodynamics of contact metamorphism
inferredcites →https://doi.org/10.1130/0091-7613(1989)017<1068:kohamv>2.3.co;2openalex-snapshot
Kinetics of hydrofracturing and metamorphic veining
inferredcites →https://doi.org/10.1130/0091-7613(1995)023<0045:paproc>2.3.co;2openalex-snapshot
Porosity and pressure: Role of compaction disequilibrium in the development of geopressures in a Gulf Coast Pleistocene basin
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The generation and dissipation of abnormal fluid pressures in active depositional environments
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Introduction To Percolation Theory
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Introduction to Percolation Theory
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Cinétiques de transition de phase dans le manteau terrestre
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