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- W1567496616 abstract "Theories on the genesis of ferruginous concretions in soils and weathering profiles continue to be debated. In particular, whether concretions represent in situ pedogenesis or are transported residues of ‘laterite’ weathering or ferricrete formation is unclear. In this study we use detailed field, micromorphological, geochemical and mineralogical investigations of a ferric soil profile from the Fraser Coast of Queensland to show that ferruginous concretions are of transported origin, and have been modified since deposition. The study found no evidence for a postulated Miocene ‘laterite’ weathering episode in this area; preserved primary minerals such as microcline show that the concretions are derived from reworked ferricrete rather than laterite." @default.
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- W1567496616 date "2010-01-01" @default.
- W1567496616 modified "2023-10-15" @default.
- W1567496616 title "Genesis of ferruginous concretions in a ferric soil and implications for past and present iron mobility" @default.
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