Abstract

The study of ore minerals is rapidly transforming due to an explosion of new micro- and nano-analytical technologies. These advanced microbeam techniques can expose the physical and chemical character of ore minerals at ever-better spatial resolution and analytical precision. The insights that can be obtained from ten of today’s most important, or emerging, techniques and methodologies are reviewed: laser-ablation inductively-coupled plasma mass spectrometry; focussed ion beam-scanning electron microscopy; high-angle annular dark field scanning transmission electron microscopy; electron back-scatter diffraction; synchrotron X-ray fluorescence mapping; automated mineral analysis (Quantitative Evaluation of Mineralogy via Scanning Electron Microscopy and Mineral Liberation Analysis); nanoscale secondary ion mass spectrometry; atom probe tomography; radioisotope geochronology using ore minerals; and, non-traditional stable isotopes. Many of these technical advances cut across conceptual boundaries between mineralogy and geochemistry and require an in-depth knowledge of the material that is being analysed. These technological advances are accompanied by changing approaches to ore mineralogy: the increased focus on trace element distributions; the challenges offered by nanoscale characterisation; and the recognition of the critical petrogenetic information in gangue minerals, and, thus the need to for a holistic approach to the characterization of mineral assemblages. Using original examples, with an emphasis on iron oxide-copper-gold deposits, we show how increased analytical capabilities, particularly imaging and chemical mapping at the nanoscale, offer the potential to resolve outstanding questions in ore mineralogy. Broad regional or deposit-scale genetic models can be validated or refuted by careful analysis at the smallest scales of observation. As the volume of information at different scales of observation expands, the level of complexity that is revealed will increase, in turn generating additional research questions. Topics that are likely to be a focus of breakthrough research over the coming decades include, understanding atomic-scale distributions of metals and the role of nanoparticles, as well how minerals adapt, at the lattice-scale, to changing physicochemical conditions. Most importantly, the complementary use of advanced microbeam techniques allows for information of different types and levels of quantification on the same materials to be correlated.

Highlights

  • IntroductionMining, processing, and refining of minerals accounts for a significant portion of global GDP

  • Mining, processing, and refining of minerals accounts for a significant portion of global GDP.Characterisation of the mineral, or in most cases minerals, making up an ore body is critical for their efficient and sustainable exploitation and for the validation and refinement of genetic models that can underpin exploration, in turn leading to new discoveries to satisfy future demand

  • We briefly review some of the recent advances in ore mineralogy—how these minerals are studied?—why they need to be studied?—and why an approach using complementary techniques gives results that can accelerate progress in understanding how the ores are formed, and why they occur where they do

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Summary

Introduction

Mining, processing, and refining of minerals accounts for a significant portion of global GDP. A good example is hematite from iron oxide-copper-gold (IOCG) deposits, such as Olympic Dam, South Australia. This contribution considers ore minerals in a loose sense, as those minerals concentrated within mineral deposits, whether of economic value or not. Examples include minerals that host lithium (Li), scandium (Sc), or the rare earth elements (REE) Such commodities may occur in traditional gangue minerals (e.g., silicates, carbonates etc.), or as trace substituents within sulphides, as in the case of indium (In) or germanium (Ge), for example. We support our conclusions by drawing upon research addressing mineralogy provides insights into understanding formation of giant ore deposits, such as the giant Olympic Dam IOCG deposit, and from Fe-Ti-oxides within layered intrusions, such as Panzhihua, southeast China. We emphasise how a combination of nanoscale techniques can offer insights into ore-forming processes and the sequence of alteration and mineralization events in these complex ore systems

Microanalytical Methods
Laser-Ablation
Focussed
Automated Mineralogy
Geochronology Using Ore Minerals
2.1.10. Non-Traditional Stable Isotopes
Trace Elements in Ore Minerals
The Significance of Gangue Minerals—A Holistic Approach to Ore Deposits
Solid Solutions and Nanoparticles
New Sub-Disciplines
Challenges—A Short Discussion
Conclusions

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