Characterization of Ore-Forming Systems from Geological, Geochemical and Geophysical Studies
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Economically viable concentrations of mineral resources are uncommon in Earth’s crust. Most ore deposits that were mined in the past or are currently being extracted were found at or near Earth’s surface, often serendipitously. To meet the future demand for mineral resources, exploration success hinges on identifying targets at depth. Achieving this requires accurate and informed models of the Earth’s crust that are consistent with all available geological, geochemical and geophysical information, paired with an understanding of how ore-forming systems relate to Earth’s evolving structure. Contributions to this volume address the future resources challenge by (i) applying advanced microscale geochemical detection and characterization methods, (ii) introducing more rigorous 3D Earth models, (iii) exploring critical behaviour and coupled processes, (iv) evaluating the role of geodynamic and tectonic setting and (v) applying 3D structural models to characterize specific ore-forming systems.
Microscale data to macroscale processes: a review of microcharacterization applied to mineral systems
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Published:January 01, 2018
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CiteCitation
Mark A. Pearce, Bélinda M. Godel, Louise A. Fisher, Louise E. Schoneveld, James S. Cleverley, Nicholas H. S. Oliver, Michael Nugus, 2018. "Microscale data to macroscale processes: a review of microcharacterization applied to mineral systems", Characterization of Ore-Forming Systems from Geological, Geochemical and Geophysical Studies, K. Gessner, T.G. Blenkinsop, P. Sorjonen-Ward
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Abstract
Microanalysis can provide rapid, quantitative characterization of mineral systems that complements the field- and core-scale observations traditionally made in ore deposits. We review recent innovations in microanalytical procedures and their application to studies of ore deposits. Case studies are presented examining how microanalysis can provide constraints on macroscopic processes within mineral systems. Synchrotron X-ray fluorescence shows centimetre-scale chemical variations associated with proximity to mineralization in samples from Sunrise Dam Gold Mine, Western Australia. Pseudomorphs of igneous plagioclase and chemically driven recrystallization interpreted from electron backscatter diffraction suggest that the system was dominated by fluid-driven brecciation with very little shearing....
- alteration
- analysis
- Australasia
- Australia
- automated analysis
- brecciation
- case studies
- cathodoluminescence
- characterization
- chemical analysis
- composition
- computed tomography
- cyclic processes
- data integration
- deformation
- electron diffraction analysis
- electron probe
- emission spectroscopy
- enrichment
- gold ores
- host rocks
- igneous rocks
- inductively coupled plasma methods
- ion probe
- komatiite
- laser ablation
- laser methods
- magmatism
- mass spectroscopy
- melts
- metal ores
- methods
- microstructure
- mineral deposits, genesis
- mineralization
- mineralogy
- nickel sulfides
- ore-forming fluids
- particle-induced X-ray emission
- petrography
- processes
- pseudomorphism
- recrystallization
- samples
- scale factor
- scale models
- scanning electron microscopy
- size distribution
- spectroscopy
- sulfides
- synchrotron radiation
- techniques
- tomography
- variations
- veins
- volcanic rocks
- Western Australia
- X-ray analysis
- X-ray fluorescence
- X-ray spectroscopy
- microanalysis
- energy-dispersive X-ray spectroscopy
- Sunrise Dam Mine
- Mount Keith Deposit