The geology of the Balcooma massive sulphide deposit, north-east Queensland

Harvey, Kenneth James (1989) The geology of the Balcooma massive sulphide deposit, north-east Queensland. Masters (Research) thesis, James Cook University.

[img]
Preview
PDF (Thesis) - Submitted Version
Download (7MB)
 
253


Abstract

The Balcooma massive sulphide deposit is located at 18°46'S, 144°43'E and 230 km west-north-west of Townsville in north Queensland. The deposit, which has reserves of 3.5 million tonnes of 3.0% copper, was discovered by the author late in 1978 during a search for volcanogenic massive sulphide deposits in the lower Palaeozoic sequences surrounding Charters Towers.

The deposit is hosted by a sequence of metamorphosed sediments and acid volcanics were referred to in this report as the "Balcooma Metamorphics". These rocks, prior to discovery of the deposit, were included in the Greenvale Subprovince and were believed to be of Precambrian age. These rocks are now interpreted to be of lower Palaeozoic age and the Greenvale Subprovince is considered to form part of the Ravenswood Lolworth Province.

The geology of the area is exceedingly complex due to at least two strong deformation events. The immediate hosts to the mineralization are a sequence of quartz muscovite biotite staurolite schists and quartz muscovite biotite schists which are interpreted to be metamorphosed fine-grained and coarse-grained sediments respectively. Quartz feldspar porphyry bodies intruded these rocks prior to deformation and metamorphism.

Both copper and lead-zinc-copper mineralization occur. Copper mineralization occurs within two south-south-west plunging shoots as chalcopyrite in massive pyrite, as massive chalcopyrite with pyrrhotite, and as chalcopyrite in chlorite schist. Chlorite alteration accompanies the copper mineralization.

Lead-zinc-copper mineralization occurs within folded tabular bodies of massive pyrite which are associated with gahnite bearing quartzite and quartz schists which are interpreted to be metamorphosed siliceous exhalites. The depositis considered to be a metamorphosed volcanogenic massive sulphide deposit.

Item ID: 28250
Item Type: Thesis (Masters (Research))
Keywords: Balcooma deposit; Greenvale subprovince; Ravenswood Lolworth Province; sulphide deposits; copper mineralisation; metamorphics; intrusions; geological exploration
Additional Information:

Thesis originally submitted in December 1984 and resubmitted in March 1989.

Date Deposited: 08 Aug 2013 06:11
FoR Codes: 04 EARTH SCIENCES > 0403 Geology > 040304 Igneous and Metamorphic Petrology @ 100%
SEO Codes: 84 MINERAL RESOURCES (excl. Energy Resources) > 8401 Mineral Exploration > 840199 Mineral Exploration not elsewhere classified @ 50%
97 EXPANDING KNOWLEDGE > 970104 Expanding Knowledge in the Earth Sciences @ 50%
Downloads: Total: 253
Last 12 Months: 23
More Statistics

Actions (Repository Staff Only)

Item Control Page Item Control Page