Search results for "weakening"

showing 3 items of 3 documents

2D Hydro-Mechanical-Chemical Modeling of (De)hydration Reactions in Deforming Heterogeneous Rock: The Periclase-Brucite Model Reaction

2020

Deformation at tectonic plate boundaries involves coupling between rock deformation, fluid flow, and metamorphic reactions, but quantifying this coupling is still elusive. We present a new two-dimensional hydro-mechanical-chemical numerical model and investigate the coupling between heterogeneous rock deformation and metamorphic (de)hydration reactions. We consider linear viscous compressible and power-law viscous shear deformation. Fluid flow follows Darcy's law with a Kozeny-Carman type permeability. We consider a closed isothermal system and the reversible (de)hydration reaction: periclase and water yields brucite. Fluid pressure within a circular or elliptical inclusion is initially bel…

010504 meteorology & atmospheric sciencesShear zoneChemical process modelingMetamorphic rockThermodynamicsNumerical simulationengineering.materialDeformation (meteorology)010502 geochemistry & geophysics01 natural sciencesPhysics::GeophysicsPhysics::Fluid DynamicsGeochemistry and PetrologyFluid dynamicsCoupling (piping)Brucite-Periclase reaction0105 earth and related environmental sciencesBruciteReaction-induced weakeningGeophysics13. Climate actionengineeringHydro-Mechanical-Chemical modelPericlaseShear zoneGeologyRock deformation coupled to reactions
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Widening of Hydrous Shear Zones During Incipient Eclogitization of Metastable Dry and Rigid Lower Crust—Holsnøy, Western Norway

2021

The partially eclogitized crustal rocks on Holsnøy in the Bergen Arcs, Norway, indicate that eclogitization is caused by the interplay of brittle and ductile deformation promoted by fluid infiltration and fluid‐rock interaction. Eclogitization generated an interconnected network of millimeter‐to‐kilometer‐wide hydrous eclogite‐facies shear zones, which presumably caused transient weakening of the mechanically strong lower crust. To decipher the development of those networks, we combine detailed lithological and structural mapping of two key outcrops with numerical modeling. Both outcrops are largely composed of preserved granulite with minor eclogite‐facies shear zones, thus representing th…

551.8fluid‐induced weakeningCrust551ddc:551.8GeophysicsGeochemistry and PetrologyMetastabilityeclogitization500 Naturwissenschaften und Mathematik::550 Geowissenschaften Geologie::551 Geologie Hydrologie Meteorologieshear zone wideningShear zoneEclogitizationPetrologyGeologyfluid‐rock interaction
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The Parallel Structures Model and the weakening of implosive /s/ in Spanish

2020

En aquest article es presenten les premisses fonamentals del Model de les Estructures Paral·leles, un model fonològic relativament recent dins el paradigma de la fonologia autosegmental, i s’aplica per primera vegada a dades de l’espanyol. En concret, el treball se centra a il·lustrar els avantatges explicatius que comporta l’adopció del Model de les Estructures Paral·leles en el cas de l’anàlisi de les realitzacions de la /s/ en posició de coda seguida d’oclusiva sorda en interior de paraula, perquè l’àmplia gamma de realitzacions documentades per a aquest context en les varietats aspirants de l’espanyol planteja un repte important per a les teories representacionals actuals sobre la compo…

CodaFonologiaModel de les Estructures Paral·leleslcsh:Comparative grammarAfeblimentCastellàEspanyolSpanishspanishlcsh:P325-325.5PhonologyphonologycodaParallel Structures Modelweakeningparallel structures model.Weakeninglcsh:P201-299lcsh:Semantics
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