Search results for "Shear zones"

showing 2 items of 2 documents

Benchmarking numerical models of brittle thrust wedges

2016

International audience; We report quantitative results from three brittle thrust wedge experiments, comparing numerical resultsdirectly with each other and with corresponding analogue results. We first test whether the participatingcodes reproduce predictions from analytical critical taper theory. Eleven codes pass the stable wedgetest, showing negligible internal deformation and maintaining the initial surface slope upon horizontaltranslation over a frictional interface. Eight codes participated in the unstable wedge test that examinesthe evolution of a wedge by thrust formation from a subcritical state to the critical taper geometry. Thecritical taper is recovered, but the models show two…

010504 meteorology & atmospheric sciencesPlasticity[SDU.STU]Sciences of the Universe [physics]/Earth SciencesThrustGeometryGeologyClassification of discontinuities010502 geochemistry & geophysics01 natural sciencesHorizontal translationWedge (geometry)Boundary frictionShear zonesCritical taperBenchmarkingCritical taperBrittlenessThrust wedgesNumerical modelling550 Earth sciences & geologyGeotechnical engineeringBoundary value problemGeology0105 earth and related environmental sciencesJournal of Structural Geology
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Fabric attractors in general triclinic flow systems and their application to high strain shear zones: A dynamical system approach

2007

High strain zones may deform by flow with a triclinic symmetry. This paper describes triclinic flow in a reference frame where Instantaneous Stretching Axes (ISA) are fixed. The operation of triclinic flow is described in two ways: first in terms of flow and the nature of flow eigenvectors and in the second part of the paper in terms of finite strain. In monoclinic flow, at least one of the eigenvectors of the flow coincides with one of the ISA and one or two of the eigenvectors act as attractors of foliation or lineation elements. In triclinic flow some flow eigenvectors are undefined since the two largest eigenvalues (controlling the flow) are imaginary. Imaginary eigenvalues are particul…

EigenvectorGeologyGeometryVorticityTriclinic crystal systemDynamical systemDeformationShear zonesPhysics::Fluid DynamicsFlow kinematicGhostvectorLineationFlow (mathematics)Finite strain theoryFoliation (geology)Eigenvalues and eigenvectorsGeology
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