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Naji, M. |
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Motta, Antonella |
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Aletan, Dirar |
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Mohamed, Tarek |
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Ertürk, Emre |
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Taccardi, Nicola |
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Kononenko, Denys |
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Petrov, R. H. | Madrid |
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Alshaaer, Mazen | Brussels |
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Bih, L. |
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Casati, R. |
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Muller, Hermance |
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Kočí, Jan | Prague |
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Šuljagić, Marija |
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Kalteremidou, Kalliopi-Artemi | Brussels |
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Azam, Siraj |
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Ospanova, Alyiya |
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Blanpain, Bart |
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Ali, M. A. |
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Popa, V. |
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Rančić, M. |
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Ollier, Nadège |
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Azevedo, Nuno Monteiro |
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Landes, Michael |
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Rignanese, Gian-Marco |
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Kilburn, Matthew
International Atomic Energy Agency
in Cooperation with on an Cooperation-Score of 37%
Topics
Publications (6/6 displayed)
- 2016The golden arkcitations
- 2015The mechanism of borosilicate glass corrosion revisitedcitations
- 2008Core formation and the oxidation state of the Earth: Additional constraints from Nb, V and Cr partitioningcitations
- 2006Examination of the influence of boron on the microstructure and properties of low C ferritic steels using NanoSIMS and TEMcitations
- 2005Effect of synovial fluid, phosphate-buffered saline solution, and water on the dissolution and corrosion properties of CoCrMo alloys as used in orthopedic implantscitations
- 2001Relative ion yields for SIMS analysis of trace elements in metallic Fe, Fe-Si alloy, and FeSicitations
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article
The golden ark
Abstract
© 2016 John Wiley & Sons Ltd. Quantitative electron backscatter diffraction analysis and ion microprobe imaging of gold-rich arsenopyrites provide the first insights into the crystal plasticity and element mobility behaviour of arsenopyrites through metamorphism (340°-460° and 2 kbar). Remarkably, the gold-rich arsenopyrites remained structurally and chemically robust during high strain deformation. It was only during a superimposed lower strain deformation event, at a high angle to the preferred orientation of the arsenopyrites, that small amounts of crystal plasticity affected the arsenopyrites. During the low strain event, a dissolution-reprecipitation reaction resulted in loss of gold from the crystal lattice, facilitated by localised domains of recrystallisation, most likely due to fluid percolation along sub- and new grain boundaries. We suggest that the abundance and rheologically robust nature of gold-rich arsenopyrite in giant gold deposits, affected by greenschist-amphibolite metamorphism, is actually critical in the preservation of those deposits.