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Variation of color, structure and morphology of fluorite and the origin of the hydrothermal F-Ba deposits at Nabburg-Wölsendorf, SE Germany

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Effect of incongruent dissolution on mineral solubility data derived from quench experiments

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On the interpretation of closed system mineral dissolution experiments: comment on ''Mechanism of kaolinite dissolution at room temperature and pressure part II: kinetic study'' by Huertas et al. (1999)

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