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    Fluorian and hydrous garnets of the regionally metamorphosed Moldanubian skarn, example from VlastÄ›jovice, Czech Republic
    Formation of extremely F-rich hydrous melt fractions and hydrothermal fluids during differentiation of highly evolved tin-granite magmas: a melt/fluid-inclusion study
    Liquidus equilibria in the system K2O-Na2O-Al2O3-SiO2-F2O-1-H2O to 100 MPa. II, Differentiation paths of fluorosilicic magmas in hydrous systems
    Removal of arsenate and selenite from aqueous solution using nano-amorphous iron-titanium hydrous oxide