CONSTRAINING THE ORIGIN AND INFLUENCE OF ANDESITE IN THE ZONED PURICO IGNIMBRITE, N. CHILE
The andesitic pumice (60 to 62% SiO2) and bands in mixed pumice are microvesicular and contain a phenocryst assemblage of plagioclase, orthopyroxene, clinopyroxene, magnetite and ilmenite ± amphibole, biotite and quartz. Glomerocrysts of opx, cpx, and plagioclase are common. Two texturally, compositionally, and isotopically distinct types of plagioclase, small (<500 μm) subhedral to euhedral crystals with high MgO (130-490 ppm) and low 87Sr/86Sr crystals (0.7076-0.7084) record a hot (>900 °C) andesite magma derived from an ~20 km deep magma reservoir. In contrast, the second type of plagioclase in the andesite appear as broken fragments of larger crystals and have significantly lower MgO (90-240 ppm), higher 87Sr/86Sr (0.7096-0.7114), and record cooler ~800-900 °C, upper crustal <10 km conditions.
The compositional variations observed in plagioclase crystals from the Purico andesitic pumices record recharge of a previously emplaced upper crustal (4-8 km depth) dacite magma reservoir by andesite coming from deep (~20 km). During ascent, the andesite incorporated crystals from the surrounding upper crustal plutonic bodies. Thus, the andesite itself is significantly modified and is a hybrid between a more mafic parent and upper crustal silicic melts.