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- W2015231611 abstract "Abstract Concentration/depth profiles of dissolved iron and silica in the pore waters of turbiditic sediments from the Nares Abyssal Plain all show a maximum at the sediment depth of 1.5–2.0 m. This uncommon phenomenon is attributable to alternating layers of organic-rich and organic-poor sediment. Diffusion of dissolved reduced iron and dissolved silica results in precipitation of an amorphous Fe-Si mineral, possibly with a clay-mineral structure, as suggested by electronmicroscopic findings." @default.
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- W2015231611 date "1986-09-01" @default.
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- W2015231611 title "Indication of a diagenetically induced precipitate of an Fe-Si mineral in sediment from the Nares Abyssal Plain, western North Atlantic" @default.
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- W2015231611 doi "https://doi.org/10.1016/0025-3227(86)90112-x" @default.
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