Economic and Environmental Geology

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Fig. 10.

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Fig. 10. (A) Homogenous distributions of some trace elements throughout three pyrite grains of type 2 from the Sheba Deposit in the, suggesting synchronous formation of these elements with pyrite, could possibly be due to background effects as well; indicating the presence of very small mineral inclusion. (B): The skewed distributions of some elements in the three pyrite grains of type 2 from the Sheba Deposit, indicating later accumulation of these elements in zones inside the pyrite by later hydrothermal solutions. These distributions reflect heterogeneity in the pyrite type 2, which is not observed by microscopy, EMPA, or LA-ICP-MS single shots.
Econ. Environ. Geol. 2021;54:213-32 https://doi.org/10.9719/EEG.2021.54.2.213
© 2021 Econ. Environ. Geol.