Magma mixing/mingling in the Eocene Horoz (Nigde) granitoids, Central southern Turkey: evidence from mafic microgranular enclaves

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dc.contributor.authorKocak, Kerim
dc.contributor.authorZedef, Veysel
dc.contributor.authorKansun, Gursel
dc.date.accessioned2020-03-26T18:15:12Z
dc.date.available2020-03-26T18:15:12Z
dc.date.issued2011
dc.departmentSelçuk Üniversitesien_US
dc.description.abstractMafic microgranular enclaves (MMEs) are widespread in the Horoz pluton with granodiorite and granite units. Rounded to elliptical MMEs have variable size (from a few centimetres up to metres) and are generally fine-grained with typical magmatic textures. The plagioclase compositions of the MMEs range from An(18)-An(64) in the cores to An(17)-An(29) in the rims, while that of the host rocks varies from An(17) to An(55) in the cores to An(07) to An(33) in the rims. The biotite is mostly eastonitic, and the calcic-amphibole is magnesio-hornblende and edenite. Oxygen fugacity estimates from both groups' biotites suggest that the Horoz magma possibly crystallised at fO(2) conditions above the nickel-nickel oxide (NNO) buffer. The significance of magma mixing in their genesis is highlighted by various petrographic and mineralogical characteristics such as resorption surfaces in plagioclases and amphibole; quartz ocelli rimmed by biotite and amphibole; sieve and boxy cellular textures, and sharp zoning discontinuities in plagioclase. The importance of magma mixing is also evident in the amphiboles of the host rocks, which are slightly richer in Si, Fe3+ and Mg in comparison with the amphiboles of MMEs. However, the compositional similarity of the plagioclase and biotite phenocrysts from MMEs and their host rocks suggests that the MMEs were predominantly equilibrated with their hosts. Evidence from petrography and mineral chemistry suggests that the adakitic Horoz MMEs could be developed from a mantle-derived, water-rich magma (> 3 mass%) affected by a mixing of felsic melt at P > 2.3 kbar, T > 730A degrees C.en_US
dc.description.sponsorshipOffice of Scientific Research [5401041]en_US
dc.description.sponsorshipThis work was financially supported by the Office of Scientific Research (Bu calisma Selcuk Universitesi Bilimsel Arastirma Projeleri tarafindan desteklenmistir. BAP; Project number: 5401041; Selcuk university; Turkey). The authors would like thank Bernard Barbarin and an anonymous reviewer for useful reviews of the manuscript and Associate Editor Ralf Milke for editorial handling.en_US
dc.identifier.doi10.1007/s00710-011-0165-7en_US
dc.identifier.endpage167en_US
dc.identifier.issn0930-0708en_US
dc.identifier.issn1438-1168en_US
dc.identifier.issue01.04.2020en_US
dc.identifier.scopusqualityQ2en_US
dc.identifier.startpage149en_US
dc.identifier.urihttps://dx.doi.org/10.1007/s00710-011-0165-7
dc.identifier.urihttps://hdl.handle.net/20.500.12395/26626
dc.identifier.volume103en_US
dc.identifier.wosWOS:000297119100009en_US
dc.identifier.wosqualityQ3en_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherSPRINGER WIENen_US
dc.relation.ispartofMINERALOGY AND PETROLOGYen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.selcuk20240510_oaigen_US
dc.titleMagma mixing/mingling in the Eocene Horoz (Nigde) granitoids, Central southern Turkey: evidence from mafic microgranular enclavesen_US
dc.typeArticleen_US

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