Melting experiments of a chondritic meteorite between 16 and 25 GPa: Implication for Na/K fractionation in a primitive chondritic Earth's mantle
Chen, Ming; El Goresy, Ahmed; Frost, Dan; Gillet, Philippe
European Journal of Mineralogy Volume 16 Number 2 (2004), p. 203 - 211
published: Mar 29, 2004
ArtNo. ESP147051602001, Price: 29.00 €
Melting experiments at high-pressure and temperature were conducted at pressures from 16 to 25 GPa using chondritic starting material but with slightly enhanced Na- and K-contents while keeping the chondritic Na/K ratio constant. The experiments revealed that majorite garnet contains enhanced concentrations of Na (3.75-4.71 wt.% Na2O) and moderately enhanced concentrations of K (0.3-0.46 wt.% K2O) from 16 to 20 GPa and it is therefore the Na- and K-bearing phase at this pressure range. The Na2O/K2O ratio (8-15) in garnet is close to the initial chondritic ratio (7) of the starting material, which might indicate that at these pressures only little Na/K fractionation takes place. At pressures above 21 GPa, the high-pressure phases enriched in Na include majorite garnet (3.08-6.22 wt.% Na2O), magnesiowüstite (1.83-3.3 wt.% Na2O), and (Mg,Fe)SiO3-perovskite (0.43-1.25 wt.% Na2O). These phases contain only small amounts of K ( 21 GPa should have taken place in the early accretional period in the primitive chondritic mantle of the Earth.