“FOUR-LETTERS” (γ → ε → β → α) THERMAL TRANSFORMATION OF Si-RICH FERRIHYDRITE
DOI:
https://doi.org/10.7494/geol.2015.41.1.121Słowa kluczowe:
γ → ε → β → α, Si-rich ferrihydrite, thermal transformation,Pobrania
Bibliografia
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Pieczara G., Rzepa G. & Gaweł A., 2014. The influence of silicate content on thermal stability of 2-line ferrihydrite and properties of its transformation products. Geology, Geophysics and Environment, 40, 1, 160–161.
Sun Z., Zhou H., Glasby G.P., Sun Z., Yang Q., Yin Z. & Li J., 2013. Mineralogical characterization and formation of Fe-Si oxyhydroxide deposits from modern seafloor hydrothermal vents. American Mineralogist, 98, 85–97.
Vempati R.K. & Loeppert R.H., 1989. Influence of structural and adsorbed Si on the transformation of synthetic ferrihydrite. Clays and Clay Minerals, 37, 273¬–279.
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