A petrological and fluid inclusion study of magnetite-scheelite skarn mineralization at Kara, Northwestern Tasmania: implications for ore genesis

The Kara magnetite-scheelite deposit is located about 40 km south of Burnie in northwestern Tasmania. The deposit consists of a number of orebodies an d the total mineable reserves are 1.7 Mt of magnetite at > 30% Fe and 0.3 M t of scheelite at 0.52% WO3. The major orebodies at Kara are hosted by the Ordovician Gordon Limestone at the southern end of the Devonian Housetop Gr anite, adjacent to the granite or separated from it by the Ordovician Moina Sandstone. At least four paragenetic stages of skarn formation and ore dep osition have been recognized: Stage I Clinopyroxene +/- garnet +/- vesuvianite +/- wollastonite +/- quart z +/- scheelite, Stage II Garnet-vesuvianite-magnetite +/- scheelite +/- apatite +/- quartz, Stage III Magnetite-amphibole-epidote-fluorite-quatz +/- chlorite +/- garne t +/- vesuvianite +/- scheelite +/- carbonate +/- pyrite +/- clinopyroxene, and Stage IV Hematite +/- fluorite st calcite +/- quartz. Fluid inclusions in clinopyroxene from Stage I homogenize at 460-620 degree sC (mode 520 degreesC). Stage II gave homogenization temperatures of 349-57 8 degreesC (mode 500 degreesC) from scheelite and 360-570 degreesC (mode 50 0 degreesC) from vesuvianite. The Stage I clinopyroxene gave a salinity ran ge of 10.0-12.0 equiv, wt.% NaCl with only one low value of 2.0 equiv. wt.% NaCl. The Stage II mineral assemblages also showed moderate salinities of 12.0 and 17.8 equiv. wt.% NaCl from scheelite and vesuvianite. Fluid inclus ions in quartz, scheelite, calcite and fluorite from the main scheelite min eralization phase, Stage III, homogenize at 230-360 degreesC with a mode at 300 degreesC and salinity varies from 0.2 to 19.8 equiv. wt.% NaCl. The mineral paragenetic and fluid inclusion studies indicate that magnetite -scheelite mineralization at Kara was formed as a proximal skarn assemblage in carbonate host. The skarn formation and ore deposition occurred in stag es starting with prograde anhydrous clinopyroxene-garnet metasomatism at re latively high temperatures, > 500 degreesC. This early assemblage was repla ced by the subsequent retrograde deposition of hydrous mineral phases (e.g. amphibole, epidote and chlorite) as temperatures decreased to 300 degreesC or less. Deposition of scheelite predominantly occurred in association with hydrous minerals (e.g. amphibole in Stage III). The high-temperature and moderate-t o-high-salinity ore fluids in early anhydrous skarn formation (Stages I and II) are consistent with fluids of magmatic origin. In comparison, the lowe r temperature and variable salinity from high (19.8 equiv. wt.% NaCl) to as low as 0.2 equiv. wt.% NaCl in Stage III suggests a possible involvement o f low-salinity meteoric waters mixing with high-salinity fluids originating from the nearby granite in the later hydrous skarn and ore formation. (C) 2001 Elsevier Science B.V. All rights reserved.