Understanding High-grade Mineralization in the Khoemacau Zone 5 Cu-Ag Deposit, Kalahari Copperbelt, NW Botswana, using μXRF Techniques
نویسندگان
چکیده
The Zone 5 Cu-Ag deposit is the most consistently (for ~4.2 km) mineralized in Khoemacau district northwestern Botswana, with an underground mineable resource of ~100 Mt grading 2 % Cu and 21 g/t Ag. consists a redox-buffered metal-zoned ore body hosted preferentially by chemically reduced meta-sediments overlying oxidized hematite-bearing arkosic sandstone. Ore-grade mineralization typically variably deformed quartz-calcite veins, along metamorphic cleavage, bedding, shear fabric, folds. Geochemical assay data established during exploration indicates widespread signifi cant concentrations Ag, correlating positively Cu. In this study, we apply Bruker M4 TORNADO micro-X-ray fluorescence (μXRF) scanner for multi-element mapping selected highgrade drill core samples, particular focus on Ag partitioning. Collection μXRF was followed microscopic SEM-EDS observations to validate results. coupled petrographic results indicate: i) multi-elemental samples very eff ective can be applied as fi rst order geochemical analytical tool characterizing targeting important sections core, ii) silicification contributed cleavage formation, which later became trap site, iii) closely associated Fe. show that native silver stromeyerite part co-precipitated hematite post Cu-(Fe)-sulfi de deposition.
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ژورنال
عنوان ژورنال: International journal of the Society of Materials Engineering for Resources
سال: 2022
ISSN: ['1347-9725', '1884-6629']
DOI: https://doi.org/10.5188/ijsmer.25.33