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<datestamp>2018-01-11</datestamp>
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<title lang=en>Fabric transitions in quartz via viscoplastic self-consistent modeling part I: Axial compression and simple shear under constant strain</title>
<creator>Morales, Luis</creator>
<creator>Lloyd, Geoffrey E.</creator>
<creator>MAINPRICE, David</creator>
<contributor>GeoForschungsZentrum - Helmholtz-Zentrum Potsdam (GFZ)</contributor>
<contributor>Institute of Geophysics and Tectonics, The University of Leeds ; Université du Québec</contributor>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Manteau et Interfaces ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<description>International audience</description>
<source>ISSN: 0040-1951</source>
<source>EISSN: 1879-3266</source>
<source>Tectonophysics</source>
<publisher>Elsevier</publisher>
<identifier>hal-01115674</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01115674</identifier>
<source>https://hal.archives-ouvertes.fr/hal-01115674</source>
<source>Tectonophysics, Elsevier, 2014, 636, pp.52-69. 〈10.1016/j.tecto.2014.08.011〉</source>
<identifier>DOI : 10.1016/j.tecto.2014.08.011</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.tecto.2014.08.011</relation>
<language>en</language>
<subject lang=en>Simple shear</subject>
<subject lang=en>Fabric transitions</subject>
<subject lang=en>VPSC</subject>
<subject lang=en>Quartz</subject>
<subject lang=en>Axial compression</subject>
<subject lang=en>Crystallographic preferred orientation</subject>
<subject>[SDU.STU.GP] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>Quartz is a common crustal mineral that deforms plastically in a wide range of temperatures and pressures, leading to the development of different types of crystallographic preferred orientation (CPO) patterns. In this contribution we present the results of an extensive modeling of quartz fabric transitions via a viscoplastic self-consistent (VPSC) approach. For that, we have performed systematic simulations using different sets of relative critical resolved shear stress of the main quartz slip systems. We have performed these simulations in axial compression and simple shear regimes under constant Von Mises equivalent strain of 100% (γ = 1.73), assuming that the aggregates deformed exclusively by dislocation glide. Some of the predicted CPOs patterns are similar to those observed in naturally and experimentally deformed quartz. Nevertheless, some classical CPO patterns usually interpreted as result from dislocation glide (e.g. Y-maxima due to prism < a > slip) are clearly not developed in the simulated conditions. In addition we reported new potential preferred orientation patterns that might happen in high temperature conditions, both in axial compression and simple shear. We have demonstrated that CPOs generated under axial compression are usually stronger that those predicted under simple shear, due to the continuous rotation observed in the later simulations. The fabric strength depends essentially on the dominant active slip system, and normally the stronger CPOs result from dominant basal slip in < a >, followed by rhomb < a > and prism [c] slip, whereas prism < a > slip does not produce strong fabrics. The opening angle of quartz [0001] fabric used as a proxy of temperature seems to be reliable for deformation temperatures of ~ 400 °C, when the main slip systems have similar behaviors.</description>
<date>2014-12-01</date>
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