Journal
AMERICAN MINERALOGIST
Volume 108, Issue 2, Pages 225-225Publisher
MINERALOGICAL SOC AMER
DOI: 10.2138/am-2022-8791
Keywords
TEM; gold; arsenic; nanoparticles
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When the LA-ICP-MS analyses of pyrite show that the gold is held within the pyrite structure, it is often based on the observation that it plots below the gold solubility line on a gold vs. arsenic plot and exhibits relatively flat counts on laser ablation time-resolved output graphs. However, the study by Ehrig et al. (2023, this issue) demonstrates through LA-ICP-MS spot analyses, transmission electron microscopy, and electron backscatter diffraction that this interpretation is not always accurate. Additionally, they use these techniques to reveal the remobilization of trace elements, including gold, in pyrite during deformation and metamorphism.
When laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) analyses of pyrite plot below the gold solubility line on a gold vs. arsenic plot and have relatively flat counts on laser ablation time-resolved output graphs, it is often interpreted that the gold is held within the pyrite structure. The study by Ehrig et al. (2023, this issue) shows, using a combination of LA-ICP-MS spot analyses of gold in pyrite, transmission electron microscopy, and electron backscatter diffraction that this is not necessarily the case. Furthermore, they use these same techniques to identify how trace elements, including gold, are remobilized in pyrite during deformation and metamorphism.
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