1992
DOI: 10.1080/08120099208728030
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Remobilization of PGE in podiform chromitite in the Coolac Serpentinite Belt, Southeastern Australia

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Cited by 8 publications
(4 citation statements)
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“…The more common Fe-Mg chlorite is usually formed at low temperatures (ca. <300 • C) [79], but the pinkish chrome chlorite in this study seems to be formed at a relatively higher temperature like~300 • C as chromium in podiform chromitites and associated mafic/ultramafic rocks would be mobilized over a range of 300-500 • C [34]. This is consistent with the estimation of fluid temperatures of at least 300 • C in the Luobusa listwanites [27].…”
Section: Formation Of the Hydrothermal Minerals And Source Of The Fluidssupporting
confidence: 79%
“…The more common Fe-Mg chlorite is usually formed at low temperatures (ca. <300 • C) [79], but the pinkish chrome chlorite in this study seems to be formed at a relatively higher temperature like~300 • C as chromium in podiform chromitites and associated mafic/ultramafic rocks would be mobilized over a range of 300-500 • C [34]. This is consistent with the estimation of fluid temperatures of at least 300 • C in the Luobusa listwanites [27].…”
Section: Formation Of the Hydrothermal Minerals And Source Of The Fluidssupporting
confidence: 79%
“…The belts are emplaced into a variety of early and middle Palaeozoic strata and are exposed over a total linear distance of 230 km (Franklin et al 1992). They vary in size from small lenses less than 5m in length, up to a single large body which crops out continuously for some 56km and are composed of variably foliated harzburgite and dunite.…”
Section: Regional Geological Settingmentioning
confidence: 99%
“…wehrlite, lherzolite) as well as talc-carbonate bodies and rodingite dykes. Podiform chromitite bodies have been found in the CSB and WSB with associated minor platinum-group element (PGE) mineralisation (Franklin et al 1992).…”
Section: Regional Geological Settingmentioning
confidence: 99%
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