AnEXTENDED ABSTRACTis available for download._x000D_
A full-length paper was notprepared for this presentation._x000D_
Key indicator hydrothermal alteration minerals formed from fluids of known fluid composition (neutral versus acid pH) and temperature have been mapped for New Zealand (NZ) geothermal fields by visible/near-infrared (VNIR) and short wave infrared (SWIR) reflectance spectroscopy. Smectite, interstratified illite-smectite and illite formed from neutral pH fluids have zoned distributions with higher temperature illite (>220C) in and around the upflow of chloride waters and low temperature smectite (<150c) on the margins (eg ohaaki, nz). in adularia-sericite epithermal deposits, au-ag veins are similarly surrounded by zoned clays, with mineralised veins enclosed by illite (eg martha, nz) or occurring at the illite illite-smectite boundary (eg favona, nz). reflectance spectroscopy is also highly effective in identifying minerals formed from acid fluids; both steam-heated acid-sulfate waters (eg kaolinite and alunite at rotokawa, nz), or magmatic-hydrothermal fluids (eg pyrophyllite and topaz at ngatamariki, nz). these same alteration minerals commonly show zoned distributions in high sulfidation epithermal deposits (eg rodalquilar, spain) and in lithocaps associated with porphyry deposits (eg lepanto, philippines). thus reflectance spectroscopy permits the rapid identification of key alteration minerals that can be mapped at a high sample frequency and used as vectors towards mineralisation.citation:simpson, m p, bignall, g, rae, a j, christie, a b and chambefort, i, 2015. mapping hydrothermal minerals in new zealand geothermal fields using reflectance spectroscopy (vnir-swir) and application to mineral deposit exploration , in proceedings pacrim 2015 congress, pp 243-248 (the australasian institute of mining and metallurgy: melbourne).>