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- W1967695280 abstract "Upper Pleistocene muds of the Amazon deep-sea fan contain an abundance of residual weathering products, as indicated by their bulk chemical and mineralogical compositions. The muds are chemically more mature than average shale, average pelagic mud, or the surrounding Demerara Abyssal sediments. They are, however, very similar to the bulk chemical compositions of contemporary suspended sediments of both the Amazon Estuary and those carried by the major Andean tributaries. The modern sediment compositions reflect the rapid weathering now occurring in the Andean source regions of the basin. The major-element geochemical signature of the Upper Pleistocene deep-sea fan sediments suggests that intense chemical weathering in the mountainous source lands has controlled the chemistry of Amazon River suspended sediments since at least the Upper Pleistocene. Minor- and trace-element signatures appear uniform throughout the fan and element concentrations are in general higher than in the intensely weathered Amazon lowland soils but lower than in deep-sea sediments." @default.
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- W1967695280 date "1986-02-01" @default.
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- W1967695280 title "Upper Pleistocene Amazon deep-sea fan muds reflect intense chemical weathering of their mountainous source lands" @default.
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- W1967695280 doi "https://doi.org/10.1016/0009-2541(86)90143-9" @default.
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