|Title:||Acigol rhyolite field, central Anatolia (part II): geochemical and isotopic (Sr–Nd–Pb, d18O) constraints on volcanism involving two high–silica rhyolite suites|
|Authors:||W. Siebel, A. K. Schmitt, E. Kiemele, M. Danisik, and F. Aydin|
|Publication:||Contrib. Mineral. Petrol., v. 162, p. 1233‐1247.|
The Acigol 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 d18O(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 eNd 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 Acigol 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.