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- W2605458125 abstract "Authigenic nontronite found on the hydrothermal silicic chimneys in the spreading center of the Mariana Trough during the SONNE cruise 57 has been investigated by means of X-ray diffractometry (XRD), differential thermal analysis (DTA), electron microscopy (TEM), infrared absorption spectroscopy (IR) and chemical analysis. The mineral is a well crystallized and mostly flake-shaped 2:1 dioctahedral clay mineral with a b-axis of about 9.10A, a dehydroxylation temperature from 365 °C to 431 °C, a layer charge higher than 0.7 and a chemical composition close to the pure Fe end member of the nontronite-beidellite series. The formation of nontronite was preliminarily discussed based on its occurrence and mineralogical and chemical properties. It was assumed that the nontronite in question might be formed by direct precipitation from hydrothermal fluid under low temperature and oxidizing conditions, and that its precipitation might happen after the formation of the amorphous silica which comprised the out-wall of the silicic chimneys." @default.
- W2605458125 created "2017-04-28" @default.
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- W2605458125 date "1992-10-10" @default.
- W2605458125 modified "2023-09-23" @default.
- W2605458125 title "Authigenic nontronite on the hydrothermal silicic chimneys in the Mariana Trough" @default.
- W2605458125 doi "https://doi.org/10.1360/yb1992-35-10-1269" @default.
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