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Publikováno v:
Earth and Planetary Science Letters. 150:381-398
Partition coefficients of Rb, Nb, La, Sr, Sm, Zr, Tm, and Y have been measured between a natural peridotite ± (TiO2 or ZrO2), its constituent minerals (olivine, clinopyroxene, orthopyroxene and accessories), and H2O-rich fluids at 2.0–3.0 GPa, 900