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Syn-depositional fault controls on the Hellyer Volcanic-hosted massive sulphide deposit

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Downs, RC (1993) Syn-depositional fault controls on the Hellyer Volcanic-hosted massive sulphide deposit. Research Master thesis, University of Tasmania.

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Abstract

Hellyer is a late-Middle Cambrian volcanic-hosted massive
sulphide deposit, situated within the Mount Read Volcanics of
western Tasmania.
The effects of post-depositional folding and wrench faulting have
been removed from the deposit to produce an interpreted Cambrian
seafloor topographic contour map. This map reveals that the
massive sulphide orebody formed within a north-south striking,
fault controlled basin. Intersections of active, syn-depositional
faults appear to have channelled hydrothermal fluids, and hence,
controlled the location of massive sulphide formation.
The most intense hydrothermal fluid flux was focussed on the
intersection of three major structural elements:-
i) north-south striking basin bounding faults,
ii) a northeast striking fault, and
iii) a northwest striking ridge.
Metal-rich stringer veins within the footwall indicate that the
orebody formed during the period of time when northeast striking
faults were actively dilating due to northwest directed
extension.
During the waning stages of the hydrothermal system, basaltic
magma rose up through a similar set of fissures and erupted onto
the seafloor, burying and preserving the deposit.

Item Type: Thesis (Research Master)
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).

Date Deposited: 15 Aug 2011 05:25
Last Modified: 15 Sep 2017 01:06
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