Geology and geochemistry of the Que River shale, Western Tasmania
Sinclair, BJ (1994) Geology and geochemistry of the Que River shale, Western Tasmania. Honours thesis, University of Tasmania.
The Que River Shale Fonnation overlies the Que-Hellyer Volcanics, which are the host
sequence to the Hellyer and Que River massive sulphide deposits, western Tasmania.
The Que River Shale is a homogeneous unit of finely laminated, fine grained (<100um)quartz, muscovite and calcite grains in a dirty brown chloritic matrix. The shale contains intercalated
resedimented volcaniclatic sandstones at the top and base of the unit. Shale composition varies by less
than 5 wt % with regards to major elements.
Deposition of the Que River Shale began after the fonnation of the Hellyer Massive sulfide
deposit but contemporaneous with the mixed sequence. Shale deposition extended throughout the end
of deposition of the Mount Charter group, synchronous with the Southwell Subgroup volcanism.
However the erruption of Upper Basalts and Andesites and the influx of predominantly rhyolitic
volcaniclastic mass-flows and turbidites associated with the Southwell Subgroup restricted the finely
laminated shale mostly to a period of quiesence between the two styles of volcanism.
The depositional environment of the Que River Shale is interpreted to represent quiet,
reducing bottom waters, due to a high proportion of complete agnostid trilobite specimems along with
the presence of carbonaceous material and pyrite nodules. Geochemical techniques have been used to
further define the basin as inhospitable (little or no oxygen present) to euxinic (free H2S). While Sisotopes
range from o34S + 17 to +43 suggesting that the sediment may have been a closed system with
respect to S04 z. ans H2S.
The Que River Shale has an andesitic provenance suggesting a local source for the shale.
However, the Que River Shale cannot be derived directly from any one source, or combination of
sources in the Mount Read Volcanics without significant modification The only quantification that
can be placed on the source rocks is that the Que River Shale must contain 20-25% Hellyer Basalt, to
obtain the high Cr values observed (up to 1.3 wt % Cr203). The Que River shale must havebeen well
homogenised by sedimentary processes to account for its restricted range in chemical composition
The Que River shale does not show an extensive alteration plume unlike the underlying
basalts. Alteration in the suite therefore cannot be used as an exploration indicator. However,
anomalous base metal values (up to 400 ppm Pb and 938 ppm Zn) are spatially association to the
orebody and may be useful as vectors to mineralisation.
|Item Type:||Thesis (Honours)|
|Additional Information:||Copyright the Author - The University is continuing to endeavour to trace the copyright owner(s) and in the meantime this item has been reproduced here in good faith. We would be pleased to hear from the copyright owner(s).|
|Deposited By:||ePrints Officer|
|Deposited On:||26 Aug 2011 12:19|
|Last Modified:||20 Oct 2012 16:01|
|ePrint Statistics:||View statistics for this ePrint|
Repository Staff Only: item control page