Types of Supergene Gold to be Expected on the Pacific Regions
    
    - Organization:
 - The Australasian Institute of Mining and Metallurgy
 - Pages:
 - 4
 - File Size:
 - 132 KB
 - Publication Date:
 - Jan 1, 1987
 
Abstract
This paper reviews some of the factors  thought to control the formation of supergene  gold in the Pacific and its Rim. Discussion  of these should lead to reassessment of the  economic potential of many areas. In several parts of the world many  gold-bearing veins display rich gold values  only in the oxidized zone, whereas beneath the  present (or ancient) watertable the unaltered  vein commonly holds only sub-economic  refractory low grade sulphides or arsenides.  In the Eastern Highlands of Australia some of  the most spectacular concentrations of - gold  have been found at shallow depths. For  example, Harper (1918) describes the Canton  mine in New South Wales which was stoped over  a length of 180 metres from the 45 metre level  to the surface. The reef yielded gold at 300  g/t in the upper levels, but became gradually  poorer at depth. Present geologists of N.S.W.  Geol. Survey, G.R. Mcllveen and B.P.J.  Stevens, believe that many similar Australian  enrichments were formed between the surface  and its ancient water table level during the  extended period of weathering in the Eocene or  pre-Eocene. They concede, however, that  further supergene movement of gold may have  occurred since the early Tertiary. Large quantities of Mesozoic supergene  gold of extreme fineness (Au 99.7%, Cu +òFe  0.3%; Leibius 1885) was found at Mt. Morgan  near the Tropic of Capricorn in Queensland.  Lower Jurassic sediments cover part of the  gossan in a small depression caused by  oxidation and collapse of the Main Pipe, thus  showing that the supergene gold is pre-Lower  Jurassic (Cornelius, 1968). Because the Lower  Jurassic landscape around Mt. Morgan was  mature with a surface slope of less than 10  (Playford and Cornelius, 1967), erosion would  have been very slow. Moreover, once all  sulphides had been removed from the ore body  the Lower Jurassic environment would have  reverted from highly acid to alkaline as it is  at present. Accordingly, gold, goethite and  1. Dept. of Geology & Mineralogy, University  of Queensland, St. Lucia, Australia,
Citation
APA: (1987) Types of Supergene Gold to be Expected on the Pacific Regions
MLA: Types of Supergene Gold to be Expected on the Pacific Regions. The Australasian Institute of Mining and Metallurgy, 1987.