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<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd> <responseDate>2018-01-15T18:22:23Z</responseDate> <request identifier=oai:HAL:hal-01355967v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-01355967v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Complete Alpine reworking of the northern Menderes Massif, western Turkey</title> <creator>CENKI-TOK, Benedicte</creator> <creator>Expert, M</creator> <creator>Isik, V.</creator> <creator>Candan, O.</creator> <creator>MONIE, Patrick</creator> <creator>BRUGUIER, Olivier</creator> <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>Dynamique de la Lithosphere ; 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>Üniversitesi Mühendislik Fak, Ankara</contributor> <source>ISSN: 1437-3254</source> <source>EISSN: 1437-3262</source> <source>International Journal of Earth Sciences</source> <publisher>Springer Verlag</publisher> <identifier>hal-01355967</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-01355967</identifier> <source>https://hal.archives-ouvertes.fr/hal-01355967</source> <source>International Journal of Earth Sciences, Springer Verlag, 2016, 105 (5), pp.1507-1524. 〈10.1007/s00531-015-1271-2〉</source> <identifier>DOI : 10.1007/s00531-015-1271-2</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1007/s00531-015-1271-2</relation> <language>en</language> <subject lang=en>Menderes Massif</subject> <subject lang=en>Metamorphic core complex</subject> <subject lang=en>U-Pb geochronology</subject> <subject lang=en>Thermochronology</subject> <subject lang=en>Amphibolite-facies metamorphism</subject> <subject>[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry</subject> <type>info:eu-repo/semantics/article</type> <type>Journal articles</type> <description lang=en>This study focuses on the petrology, geochronology and thermochronology of metamorphic rocks within the northern Menderes Massif in western Turkey. Metasediments belonging to the cover series of the Massif record pervasive amphibolite-facies metamorphism culminating at ca. 625–670 °C and 7–9 kbars. U–Th–Pb in situ ages on monazite and allanite from these metapelites record crustal thickening and nappe stacking associated with the internal imbrication of the Anatolide–Taurides platform during the Eocene. In addition, new 39Ar/40Ar single muscovite grain analyses on deformed rocks were performed in three localities within the northern Menderes Massif and ages range from 19.8 to 25.5 Ma. These mylonites may be related to both well-known detachments, Simav to the north and Alaşehir to the south, which accommodate Oligo–Miocene exhumation of the Menderes core complex. U–Th–Pb data on monazite grains (22.2 ± 0.2 Ma) from migmatites emplaced within the Simav detachment confirm these ages.</description> <date>2016-07</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>