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<identifier>oai:HAL:hal-00824537v1</identifier>
<datestamp>2018-01-11</datestamp>
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<metadata><dc>
<publisher>HAL CCSD</publisher>
<title lang=en>Kinematic and temporal relationships between parallel fold hinge lines and stretching lineations: A microstructural and crystallographic preferred orientation approach</title>
<creator>Morales, Luis</creator>
<creator>Casey, Martin</creator>
<creator>Lloyd, Geoffrey E.</creator>
<creator>Williams, Danielle M.</creator>
<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>
<contributor>University of Leeds</contributor>
<source>ISSN: 0040-1951</source>
<source>EISSN: 1879-3266</source>
<source>Tectonophysics</source>
<publisher>Elsevier</publisher>
<identifier>hal-00824537</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00824537</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00824537</source>
<source>Tectonophysics, Elsevier, 2011, 503 (3-4), pp.207-221. 〈10.1016/j.tecto.2011.03.003〉</source>
<identifier>DOI : 10.1016/j.tecto.2011.03.003</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.tecto.2011.03.003</relation>
<language>en</language>
<subject lang=en>Folds</subject>
<subject lang=en>Shear zones</subject>
<subject lang=en>CPO</subject>
<subject lang=en>EBSD</subject>
<subject lang=en>Western Internal Alps</subject>
<subject>[SDU.STU.PE] Sciences of the Universe [physics]/Earth Sciences/Petrography</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>Folds with hinge lines subparallel to stretching lineation are common features in shear zones and represent extreme cases of fold modification. However, their microstructures and in particular their kinematic significance remain poorly understood. Here we describe the meso- and micro-scale structures and crystallographic preferred orientation (CPO) of quartz and muscovite from a metric-scale shear-modified fold from Plattjen, Saas Fee, Western Internal Alps. The studied fold is of class-2 and the samples collected around the fold have essentially the same microstructures. Quartz [c]-axes plotted in the tectonic coordinate system exhibit an apparent reverse obliquity on opposing limbs. Muscovite fabrics are controlled essentially by the orientation of {001} planes. If the CPO data are plotted in a common reference frame (e.g. either fold or geographical), all samples exhibit essentially the same patterns for both minerals. In particular, relative to the fold axis and axial surface, the reversal of quartz CPO obliquity on opposing limbs is no longer evident. The small obliquity (~ 15°) between the intersection lineation of the two planes of {001} of muscovite and the fold axis results in the apparent reversal of shear sense on opposite limbs when viewing the CPO related to the macroscopic fabric. The homogeneity of the microstructures and CPOs of quartz and muscovite across the fold support the interpretation that the fold developed during simultaneous activation of heterogeneous and homogeneous simple shear, with the former responsible for fold development and the latter responsible for fold rotation and the overwhelming of the heterogeneous deformation. These processes led to the observed parallelism between fold hinge line and local stretching lineation.</description>
<date>2011-04-29</date>
</dc>
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