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dc.contributor.authorGursu, Semih
dc.date.accessioned2020-11-20T15:02:38Z
dc.date.available2020-11-20T15:02:38Z
dc.date.issued2016
dc.identifier.issn0301-9268
dc.identifier.issn1872-7433
dc.identifier.urihttps://doi.org/10.1016/j.precamres.2016.01.025
dc.identifier.urihttps://hdl.handle.net/20.500.12809/2558
dc.descriptionGoncuoglu, M. Cemal/0000-0002-4216-6995en_US
dc.descriptionWOS: 000371841600027en_US
dc.description.abstractA new petrogenetic model is presented for genesis of the Late Neoproterozoic meta-granitic rocks in the central and southern Menderes Massif (MM). This study evaluates the Sr and Nd isotope geochemistry of 12 meta-granite rock samples collected from the central and southern MM to constrain the late-stage evolution of the Cadomian Orogeny in western Turkey. LA-ICP-MS analyses in the literature yield an age interval of 544.9-554.4 Ma for crystallization of the meta-granitic rocks in the MM, western Turkey. The meta-granitic rocks are classified as augen gneisses, bi-rich granitic mylonites that are cross-cut by trm-rich granitic mylonites. Geochemically, the biotite-rich granitic mylonites and augen gneisses have high HFSE and HREE-enriched multi-elemental patterns, whereas tourmaline-rich granitic mylonites display less enriched HFSE and LREE, with negative anomalies in Nb, Ti and Eu. The studied rocks are not juvenile and have a crustal component and residence history based on the initial Nd-143/Nd-144((t)) (0.51169-0.51190) ratios and negative epsilon Nd-(t) (-4.63 to -0.54) values. The geochemical trends of the four biotite-rich granitic mylonite samples and three augen gneiss samples indicate that they may have been derived from mafic sources followed by mixing of a continental crust source. In contrast, the five trm-rich granitic mylonites display no mixing effect of upper continental crust in their genesis. The secondary, intense alteration/fluid-ingress process strongly changed the primary geochemical features of these rocks during or after mylonitization. The Sm-147/Nd-144 ratios of the four bi-rich granitic mylonite samples and three augen gneiss samples have typical crustal values (0.12-0.13). In contrast, four of the five trm-rich granitic mylonite samples yield Sm-147/Nd-144 ratio ranges of 0.20-0.28 (the fifth trm-rich granitic mylonite sample yielded a value of 0.12). The 0.20-0.28 Sm-147/Nd-144 ratios are higher than crustal values. All three rock suites may have been emplaced during late- to post-collisional back-arc extension at 545-560 Ma behind the Cadomian arc concomitant with southward subduction of the Proto-Tethys Ocean along the northern margin of Gondwana. This has also been observed in the peri-Gondwanan terranes in W and E Europe, Iran, Tibet and SE Asia. (C) 2016 Elsevier B.V. All rights reserved.en_US
dc.item-language.isoengen_US
dc.publisherElsevieren_US
dc.item-rightsinfo:eu-repo/semantics/closedAccessen_US
dc.subjectLate Neoproterozoicen_US
dc.subjectMeta-Granitic Rocksen_US
dc.subjectMenderes Massifen_US
dc.subjectLate To Post-Collisionen_US
dc.subjectI-Typeen_US
dc.subjectCadomian Orogenyen_US
dc.titleA new petrogenetic model for meta-granitic rocks in the central and southern Menderes Massif - W Turkey: Implications for Cadomian crustal evolution within the Pan-African mega-cycleen_US
dc.item-typearticleen_US
dc.contributor.departmenten_US
dc.contributor.departmentTemp[Gursu, Semih] Univ Kansas, Dept Geol, IGL, Lawrence, KS 66045 USA -- [Gursu, Semih] Mugla Sitki Kocman Univ, Ankara, Turkeyen_US
dc.identifier.doi10.1016/j.precamres.2016.01.025
dc.identifier.volume275en_US
dc.identifier.startpage450en_US
dc.identifier.endpage470en_US
dc.relation.journalPrecambrian Researchen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US


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