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<identifier>oai:HAL:hal-00412183v1</identifier>
<datestamp>2018-01-11</datestamp>
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<publisher>HAL CCSD</publisher>
<title lang=en>New age constraints on emplacement of the cevenol granitoids, south french massif central</title>
<creator>Brichau, S.</creator>
<creator>Respaut, Jean-Patrick</creator>
<creator>Monie, Patrick</creator>
<contributor>School of Earth Sciences, University and Birkberck College, London ; 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>
<description>International audience</description>
<source>ISSN: 1437-3254</source>
<source>EISSN: 1437-3262</source>
<source>International Journal of Earth Sciences</source>
<publisher>Springer Verlag</publisher>
<identifier>hal-00412183</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00412183</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00412183</source>
<source>International Journal of Earth Sciences, Springer Verlag, 2008, 97 (4), pp.725-738. 〈10.1007/s00531-007-0187-x〉</source>
<identifier>DOI : 10.1007/s00531-007-0187-x</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1007/s00531-007-0187-x</relation>
<language>en</language>
<subject lang=en>U-Pb</subject>
<subject lang=en>Ar-40/Ar-39</subject>
<subject lang=en>granites</subject>
<subject lang=en>Cevennes</subject>
<subject lang=en>French Massif Central</subject>
<subject lang=en>Para-autochthonous domain</subject>
<subject lang=en>tectonic evolution</subject>
<subject lang=en>hercynian granitoids</subject>
<subject lang=en>accessory minerals</subject>
<subject lang=en>Montagne Noire</subject>
<subject lang=en>France</subject>
<subject lang=en>zircon</subject>
<subject lang=en>Pyrenees</subject>
<subject lang=en>temperature</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<subject>[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>During the development of the Variscan orogeny, large amounts of granitic melt were produced, giving rise to the intrusion of granitoids at different structural levels. Despite numerous studies, ages available from previous work on the Cevennes granites remain largely imprecise. In order to better constrain the age and emplacement mode of these granites, we have combined U-Pb dating on monazites and zircons and Ar-40/Ar-39 dating on biotites with petrological observations, major element chemical analysis and SEM zircon imaging on five samples from the Aigoual-St Guiral-Liron and Mont Lozere granitic massifs. The results revealed that granitic intrusions and cooling in Southern Cevennes occurred in a short time span at similar to 306 Ma after the main episode of regional metamorphism. Petrological and chemical data suggest that they result from a mixing between mantle-derived basic magmas (lamprophyres) and lower crust acid magmas. At a regional scale the production of these melts occurred at the end of crustal thickening induced by nappe stacking, at the same time as the late anatectic events recorded further north in the Velay dome and the granulite facies metamorphism recorded in metasedimentary granulite enclaves brought up by Tertiary volcanoes of the Velay area (Bournac).</description>
<date>2008</date>
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