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Vermiculite Magnetic Separation

X-ray diffraction, FTIR, and chemical analyses were performed on clay fractions 12 m, lt0.1 m, separated by means of size fractionations and high-gradient magnetic separation techniques, from a Cryorthod developed in a chlorite-mica schist saprolite. Weathering of large phyllosilicates pre-existing in the saprolite involves physical fragmentation and mineralogical transformations.

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