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- W2016446002 abstract "Abstract Phosphatic crusts and nodules recovered from the continental margin off Peru did not precipitate authigenically from anoxic pore water but were formed in post-Palaeogene times by phosphatisation of quartzitic and feldspathic carbonate-bearing sediments. The late Quaternary uranium-series and amino acid dates obtained for these phosphatic rocks are probably the result of secondary enrichment of organic matter and uranium and probably do not represent the times of phosphate mineralisation." @default.
- W2016446002 created "2016-06-24" @default.
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- W2016446002 date "1983-01-01" @default.
- W2016446002 modified "2023-09-27" @default.
- W2016446002 title "Offshore Peruvian phosphorite: A reappraisal of its age and genesis" @default.
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- W2016446002 doi "https://doi.org/10.1016/0009-2541(83)90047-5" @default.
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