Abstract

This study documents the bulk Au fineness (Au parts per thousand) of the bullion from a placer gold mine in southern New Zealand. The compositions of doré bars produced approximately every 10 days over nearly three years is compared to the range of compositions of gold particles which have been extracted. Silver is the principal impurity in the gold, and the doré bars contained 2–3 wt % Ag over the period examined. At the scale of a typical individual 0.5 mm gold particle, there are three different types of gold: an Ag-bearing core (2–9 wt % Ag), a 10–50 µm wide Ag-poor rim (typically <1 wt % Ag), and micron scale overgrowth gold (0% Ag). The overgrowths are volumetrically negligible, and the average Ag content of a gold particle is controlled principally by the proportions of core and rim gold. The rims have been formed by recrystallisation of deformed core gold, with associated leaching of the Ag from the recrystallised gold. The volumetric proportion of cores has decreased with increasing flattening of gold particles, and highly flattened and folded flakes have little or no remnant cores. The bulk Au fineness of doré bars from the mine has decreased from ~980 to ~970 as the mine progressed upstream in a Pleistocene paleochannel because the upstream gold has been less flattened than the downstream gold.

Highlights

  • Metallic gold in mineral deposits generally contains other metals in addition to Au, especially silver (Ag), as natural amalgams [1,2,3,4]

  • To examine the detailsofofgold the internal structure of ensure the flakes, blocks produced by sprinkling subsamples on to sticky tape to thatmounting most flakes werewere at least partly by sprinkling subsamples of gold on to sticky tape to ensure that most flakes were at least partly standing on an edge, embedding the flakes in resin

  • Au fineness fineness of of the the product product of of aa mining mining operation operation is is reflected reflected in in the the composition composition of of the the gold bars poured on a mine site

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Summary

Introduction

Metallic gold in mineral deposits generally contains other metals in addition to Au, especially silver (Ag), as natural amalgams [1,2,3,4]. The principal on-site products of gold mining operations are doré bars formed from the melting of concentrated gold, and the Au fineness of these doré bars reflects the average bulk Au fineness of the ore [2]. This average bulk Au fineness may be different from that observed in individual gold particles observed at the hand specimen scale at the exploration stage because of geologically-driven variability in the bulk ore. There is a need for geometallurgical studies of the relationships between the different observational scales of Au fineness: single gold particles versus bulk mine products

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