Experimental constraints on the thermodynamic modelling of siderophile element distribution during core-segregation and basalt petrogenesis
In order to effectively model the partitioning behaviour of siderophile elements during processes ranging from planetary differentiation in the early solar system to contemporary examples of igneous petrogenesis, we require an accurate determination of the physiochemical variables that control their distribution between phases. An X-ray absorption near edge structure (XANES) spectroscopic study of silicate glasses, synthesized at high pressure and quenched isobarically, has been conducted in...[Show more]
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