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dc.contributor.authorSiebel, Wolfgang
dc.contributor.authorSchmitt, Axel K.
dc.contributor.authorKiemele, Elena
dc.contributor.authorDanišík, Martin
dc.contributor.authorAydin, Faruk
dc.date.accessioned2011-08-11T21:58:57Z
dc.date.available2011-08-11T21:58:57Z
dc.date.issued2011
dc.identifier.citationSiebel, W., Schmitt, A.K., Kiemele, E., Danišík, M. & Aydin, F. (2011). Acigöl rhyolite field, central Anatolia (part II): geochemical and isotopic (Sr–Nd–Pb, δ¹⁸O) constraints on volcanism involving two high-silica rhyolite suites. Contributions to Mineralogy and Petrology, available online on 07 June 2011.en_NZ
dc.identifier.urihttps://hdl.handle.net/10289/5566
dc.description.abstractThe Acigöl rhyolite field erupted the most recent high-silica rhyolites within the Cappadocian Volcanic Province of central Anatolia, Turkey. It comprises two sequences of domes and pyroclastic rocks with eruption ages of ∼150–200 ka (eastern group) and ∼20–25 ka (western group). Compositionally, the eastern rhyolite group lavas are less evolved (SiO₂ = 74–76 wt%), whereas the western group has higher silica abundance (SiO₂ = ∼77 wt%) with extremely depleted feldspar-compatible trace elements. Within each group, compositional variability is small and ¹⁴³Nd/¹⁴⁴Nd (0.51257–0.51265) and Pb isotope compositions (²⁰⁶Pb/²⁰⁴Pb = 18.87–18.88, ²⁰⁷Pb/²⁰⁴Pb = 15.65–15.67 and ²⁰⁸Pb/²⁰⁴Pb = 38.94–38.98) are homogeneous. The western group rhyolites have δ¹⁸O(zircon) overlapping mantle values (5.7 ± 0.2%), whereas eastern group rhyolites are enriched in d18O by ∼ 0.5%, consistent with a tendency to lower εNd values. By contrast, western group rhyolites have markedly more radiogenic ⁸⁷Sr/⁸⁶Sr ratios (0.7065–0.7091) compared to those of the eastern group (0.7059–0.7065). The presence of angular granitic xenoliths and a correlation between hydration (based on loss on ignition data) and ⁸⁷Sr/⁸⁶Sr in the western lavas, however, indicates that Sr was added during the eruption or posteruption alteration. Isotope constraints preclude the possibility that the rhyolite magmas formed by partial melting of any known regional crystalline basement rocks. Basalts and andesites erupted in the periphery of the Acigöl field are characterised by ⁸⁷Sr/⁸⁶Sr ratios between 0.7040 and 0.7053, ¹⁴³Nd/¹⁴⁴Nd = 0.51259–0.51300, ²⁰⁶Pb/²⁰⁴Pb = 18.85– 18.87, ²⁰⁷Pb/²⁰⁴Pb = 15.646–15.655, ²⁰⁸Pb/²⁰⁴Pb =38.90–38.97. The isotopic and trace element data favour an origin of the rhyolites by mixing of basaltic/andesitic magmas with minor amounts of crustal melts and followed by extensive fractional crystallization.en_NZ
dc.language.isoen
dc.publisherSpringeren_NZ
dc.relation.urihttp://www.springerlink.com/content/f667v645n73260m5/en_NZ
dc.subjectAcigölen_NZ
dc.subjectδ¹⁸O in zirconen_NZ
dc.subjectRhyoliteen_NZ
dc.subjectSilicic volcanismen_NZ
dc.subjectSr–Nd–Pb isotopesen_NZ
dc.titleAcigöl rhyolite field, central Anatolia (part II): geochemical and isotopic (Sr–Nd–Pb, δ¹⁸O) constraints on volcanism involving two high-silica rhyolite suitesen_NZ
dc.typeJournal Articleen_NZ
dc.identifier.doi10.1007/s00410-011-0651-2en_NZ
dc.relation.isPartOfContributions to Mineralogy and Petrologyen_NZ
pubs.begin-page1en_NZ
pubs.elements-id36218
pubs.end-page15en_NZ
pubs.issue6en_NZ
pubs.volumeonlineen_NZ


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