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Minerals in the arrojadite, alluaudite and jahnsite – whiteite groups from the Mount Wills pegmatite field, Victoria, Australia

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Complex assemblages of Fe– Mn phosphate minerals occur in several granitic pegmatites in the Mount Wills region of Northeastern Victoria, Australia. The Blue Jacket and Knocker dykes are the most fractionated in the pegmatitefield derived from late-stage melts of the Late Silurian Mount Wills Granite. The phosphates include members of the arrojadite, alluaudite and jahnsite– whiteite groups, most commonly formingfine-grained intergrowths that have replaced primary phases such as triplite, wolfeite and presumed triphylite. Electron microprobe analysis has enabled the identification of a range of species, based on new nomenclature schemes for the three main groups of Fe–Mn phosphates present in the pegmatites.
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Keywords: ALLUAUDITE; ARROJADITE; FE–MN PHOSPHATES; GRANITE PEGMATITE; JAHNSITE–WHITEITE; MOUNT WILLS; VICTORIA

Document Type: Research Article

Publication date: June 1, 2018

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  • The European Journal of Mineralogy publishes original papers, review articles and letters dealing with the mineralogical sciences s.l. These include primarily mineralogy, petrology, geochemistry, crystallography and ore deposits, as well as environmental, applied and technical mineralogy. Nevertheless, papers in any related field, including cultural heritage, will be considered.
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