Abstract
The hypothesis that the extent of geochemical evolution of lateritic iron oxides gives an indication of the relative age of the laterite is tested on a vertical profile in a gold mine near Kalgoorlie using Mössbauer spectroscopy and X-ray diffraction. No correlation between the structural or compositional properties of the iron oxides and their depth in the profile is found.
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Pierre, T.G.S., Webb, J. & Butt, C.R.M. Lateritic mineralization near Kalgoorlie, Western Australia: Dating by Mössbauer spectroscopy?. Hyperfine Interact 57, 2279–2283 (1990). https://doi.org/10.1007/BF02405800
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DOI: https://doi.org/10.1007/BF02405800