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- W2090254002 abstract "Samples of surface metalliferous sediment recovered from the crest of the East Pacific Rise at 6°S and 10°S latitudes and from the adjacent Bauer Basin are characterized by an authigenically formed, Fe-rich montmorillonite that dominates the non-carbonate mineralogy of the clay fraction (< 2 μm). Oxygen-isotopic formation temperatures indicate that the Fe-montmorillonites are created by low-temperature, hydrothermal processes (30°–50°C) in the 10°S region of the East Pacific Rise and Bauer Basin, possibly as a result of cooling and oxidation of unstable, high-temperature (380° ± 30°C) sulfide assemblages or as a result of the percolation of hydrothermally altered seawater solutions through underlying basalt and sediments. The widespread sedimentation of the clay mineral is suggested to be caused by colloidal transport, possibly as a result of erosion of hydrothermal mounds by bottom currents. Hydrothermal Fe-montmorillonite-nontronite formation may act as a direct and significant oceanic sink for Si and Fe released by the high-temperature, hydrothermal alteration of basalt at ocean spreading centers." @default.
- W2090254002 created "2016-06-24" @default.
- W2090254002 creator A5030166584 @default.
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- W2090254002 date "1981-01-01" @default.
- W2090254002 modified "2023-10-16" @default.
- W2090254002 title "Hydrothermal clay mineral formation of East Pacific rise and Bauer Basin sediments" @default.
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- W2090254002 doi "https://doi.org/10.1016/0009-2541(81)90143-1" @default.
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