新南威尔士州Bimbimbie金矿的含金褐铁矿钟乳石

L. Lawrence
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引用次数: 0

摘要

Bimbimbie金矿位于新南威尔士州Batemans Bay西南11公里处的同构造花岗岩块中,该块侵入了奥陶纪的变质沉积层。矿区内有三条金-黄铁矿石英脉,其中最大的一条为Bimbimbie脉,是主要产地。在一个大型采场的背面进入Bimbimbie矿脉大量褐铁矿(针长石)钟乳石出现。其中两种样品的金含量分别为26.1ppm和16.2ppm。导致金在这些钟乳石中掺入的化学过程是根据金在硫代硫酸盐离子中的溶解度来考虑的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Auriferous Limonitic Stalactites from the Bimbimbie Gold Mine, New South Wales
The Bimbimbie gold mine is situated within a syntectonic granite mass that intrudes Ordovician metasediments 11 km south-west of Batemans Bay, NSW. Three gold-pyrite quartz veins occur within the mine area, the largest - the Bimbimbie vein - being the main producer. On the backs of a large stope into the Bimbimbie vein numerous limonitic (goethitic) stalactites occur. Two of these were assayed for gold giving 26.1ppm and 16.2ppm respectively. The chemistry of the process leading to the incorporation of gold in these stalactites is considered in terms of the solubility of gold in the thiosulphate ion.
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