Copy the page URI to the clipboard
Wilson, C. J. N.; Charlier, B. L. A.; Fagan, C. J.; Spinks, K. D.; Gravley, D. M.; Simmons, S. F. and Browne, P. R. L.
(2010).
DOI: https://doi.org/10.1016/j.jvolgeores.2008.04.010
Abstract
Recognition and correlation of rock units within geothermal fields is often hampered by high degrees of alteration that obscure primary mineralogies and lithological boundaries and preclude direct dating by radiometric techniques. Magmatic zircons are commonly present in silicic volcanic rocks, where zircon saturation was achieved and zircons crystallized up to the point of eruption. Young zircons are highly resistant to hydrothermal alteration and can yield a record of their crystallization ages in otherwise heavily altered rocks. Zircon crystallization age spectra have been obtained from three samples of cuttings and a core sample from ignimbrite penetrated in 3 drillholes up to ~3.2 km deep at the Mangakino geothermal field in New Zealand. The crystallization ages are similar between the drillcore and cuttings samples, indicating that downhole mixing of cuttings has not been important, and showing collectively that volcanic units of closely similar ages are represented between ~1.4 and ~3.2 km depth. This is despite apparent changes in the inferred primary volcanic lithology that had led to earlier inferences that multiple ignimbrites of contrasting age were present in this depth interval. Comparisons of zircon crystallization age spectra and inferred primary mineralogical characteristics from the drillhole samples with surficial ignimbrites that crop out west of Mangakino suggest that the boreholes have entered a >1.8-km-thick intracaldera fill of ignimbrite generated in the closely-spaced Kidnappers and Rocky Hill eruptions at ~1 Ma.
CORE (COnnecting REpositories)
CORE (COnnecting REpositories)
