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<publisher>HAL CCSD</publisher>
<title lang=en>Late orogenic exhumation of the Variscan high-grade units (South Armorican Domain, western France), combined structural and 40Ar/39Ar constraints</title>
<creator>Turrillot, Paul</creator>
<creator>Augier, Romain</creator>
<creator>Monié, Patrick</creator>
<creator>Faure, Michel</creator>
<contributor>Institut des Sciences de la Terre d'Orléans (ISTO) ; Institut national des sciences de l'Univers (INSU - CNRS) - Université d'Orléans (UO) - Université François Rabelais - Tours - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Bureau de Recherches Géologiques et Minières (BRGM) (BRGM)</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>
<description>International audience</description>
<source>ISSN: 0278-7407</source>
<source>Tectonics</source>
<publisher>American Geophysical Union (AGU)</publisher>
<identifier>insu-00628699</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-00628699</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-00628699/document</identifier>
<identifier>https://hal-insu.archives-ouvertes.fr/insu-00628699/file/2010TC002788.pdf</identifier>
<source>https://hal-insu.archives-ouvertes.fr/insu-00628699</source>
<source>Tectonics, American Geophysical Union (AGU), 2011, 30 (TC5007), pp.1-27. 〈10.1029/2010TC002788〉</source>
<identifier>DOI : 10.1029/2010TC002788</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1029/2010TC002788</relation>
<language>en</language>
<subject lang=en>variscan high-grade units</subject>
<subject lang=en>Ar/Ar dating</subject>
<subject lang=en>Armorican Massif</subject>
<subject lang=en>South Armorican Domain</subject>
<subject lang=en>exhumation constraints</subject>
<subject lang=en>stretching continuum</subject>
<subject lang=en>variscan high-grade units.</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The current structure of the South Armorican Domain in the French Variscan Belt, provides an excellent record of the late orogenic evolution, as documented by the complex interactions between extensional structures and partial melting. In the Golfe du Morbihan, the South Brittany Migmatite Belt (SBMB), tectonically overlain by non-melted metamorphic units, was studied by combined structural and 40Ar/39Ar methods. The recognition of successive deformation stages points to a strain continuum initiated at depth at the end of a partial melting event, and continued to near-surface brittle faulting, encompassing ductile strain localization over a major top-to-the-ESE extensional shear zone (SSZ) consistent with an overall WNW-ESE orogen-parallel stretching. This multidisciplinary study making the link between structure, texture, microchemistry and 40Ar/39Ar geochronology allow distinguishing between cooling, recrystallization and syn-tectonic crystallization ages. The first extensional insights, witnessed by dyke intrusion were dated at ~319 ± 6 Ma immediately after the SBMB partial melting. Strain localization along the SSZ, occurred until ~302-298 Ma when SBMB crossed the ductile-brittle transition. Moreover, in situ 40Ar/39Ar analysis, of syn-tectonic white micas sampled in the ductile and brittle structures yield similar ~300 Ma. Formation or reactivation of the SSZ may have occurred during the rapid cooling of the SBMB settled at ~305 Ma by conventional 40Ar/39Ar analysis. Large-scale late orogenic extensional event of the previously overthickened Variscan crust thus lasted over ~20 ± 3 Myr in the same extensional tectonic regime guided by the South Armorican Shear Zone.</description>
<date>2011</date>
</dc>
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