Radium and other trace element partition coefficients have been experimentally determined for plagioclase and alkali-feldspar in equilibrium with silicate melts. In anorthitic plagioclase, alkalis (e.g. Na, K, Rb, Cs) and the heavy earth alkalis (e.g. Ba, Ra) are incompatibles, in albitic plagioclase Na is compatible, whereas Ca and Sr are always compatible in plagioclase. D_Ra^{plagioclase/melt} was determined to be 0.017 ± 0.006 (An₉₁), 0.025 ± 0.009 (An₈₁) and 0.47 ± 0.08 (An₃₄) for three different An contents, the ratio D_Ra/D_Ba increasing with decreasing An component. In alkali-feldspar, K, Rb, Ba, Ra, and Sr are compatible, whereas Na, Cs, and Ca are incompatible. D_Ra^{alkali-feldspar/melt} was determined to 2.54 ± 0.04 for a Or₇₅Ab₂₁An₄ composition, the ratio D_Ra/D_Ba is 0.55 ± 0.01. For plagioclase, D_Ra and X_An are related as RT lnD_Ra [kJ/mol] = -52.54(± 5.75)X_An -4.25(± 1.51) and D_Ra/D_Ba = exp((-9.47(± 6.21)X_An -13.66(± 1.52))/RT) [kJ/mol], allowing calculation of D_Ra from the An content of magmatic plagioclase. For alkali-feldspar we propose the equation D_Ra/D_Ba = exp((-16.06(± 0.58) +15.52(± 0.67) X_Or)/RT) [kJ/mol]. The experimentally determined partition coefficients are then used to recalculate Th-Ra-Ba model ages, leading to generally shorter feldspar residence times. The variations encompass 20 to 90% shorter crystallization ages with respect to the originally calculated ones, in two cases feldspar crystallization ages increase slightly. For several cases the measured plagioclase and melt have either never been in equilibrium or the Th-Ra-Ba system has been disturbed after crystallization.