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Does tungsten availability control the presence of tungsten in turbidite-hosted orogenic gold mineralization? Evidence from the meguma and Bendigo-Ballarat Terranes

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Cave, BJ, Large, RR, White, CE and McKnight, S 2017 , 'Does tungsten availability control the presence of tungsten in turbidite-hosted orogenic gold mineralization? Evidence from the meguma and Bendigo-Ballarat Terranes' , Canadian Mineralogist, vol. 55, no. 6 , pp. 973-999 , doi: 10.3749/canmin.1600088.

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Abstract

Turbidite-hosted orogenic Au deposits are commonly enriched in W, along with a variety of other trace elements. A mineralogical source for W has recently been shown in the Otago Schist of southern New Zealand (Cave et al. 2016), with detrital rutile in the metasedimentary rocks recrystallizing to metamorphic titanite and making W available to be mobilized from the rock mass. In this study, we investigate the availability of W through prograde metamorphic mineral recrystallization in two additional turbidite-hosted orogenic Au provinces, one containing orogenic Au mineralization with associated subordinate W (Meguma Terrane, Canada), and the other containing orogenic Au mineralization without associated W (Bendigo-Ballarat Terrane, Australia). This was undertaken to assess whether W availability during prograde metamorphism is a key process in controlling the presence of W in turbidite-hosted orogenic Au mineralization. Like the Otago Schist, in both terranes detrital rutile is identified as being the most important host mineral for W in the lowest metamorphic grade rocks, and its prograde metamorphic recrystallization (to ilmenite) makes significant amounts of W available for mobilization (0.65 and 1.85 g of W per tonne of rock from the Goldenville and Halifax groups of the Meguma Terrane, respectively, and 0.16 g of W per tonne of rock from the Castlemaine Group of the Bendigo-Ballarat Terrane). This release of W in the Meguma Terrane is likely the source of W in these orogenic Au deposits. The lack of W in the orogenic Au deposits of the Bendigo-Ballarat Terrane suggests that W availability is not the only process controlling the presence of W minerals in turbidite-hosted orogenic Au mineralization. Alternatively, it might reflect a lower greenschist facies metasedimentary (Castlemaine Group) source for these deposits (i.e., a lower metamorphic grade source than the rutile to ilmenite conversion), as has been previously suggested.

Item Type: Article
Authors/Creators:Cave, BJ and Large, RR and White, CE and McKnight, S
Keywords: Bendigo-Ballarat Terrane, coupled dissolution-re-precipitation processes, ilmenite, Meguma Terrane, metal availability, metals source, mineral recrystallization, orogenic gold, rutile, tungsten
Journal or Publication Title: Canadian Mineralogist
Publisher: Mineralogical Assoc Canada
ISSN: 0008-4476
DOI / ID Number: 10.3749/canmin.1600088
Copyright Information:

Copyright 2017 Mineralogical Association of Canada

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