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arXiv · 1812.10276

The effect of diffusive re-equilibration time on trace element partitioning between alkali feldspar and trachytic melts

Fabio Arzilli·Alessandro Fabbrizio·M. W. Schmidt·Maurizio Petrelli·M Maimaiti·D. B. Dingwell·E. Paris·M. Burton·M. Carroll
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Abstract

We present new experimental data on major and trace element partition coefficients between alkali feldspar and trachytic melt. Experiments were conducted at 500 MPa, 870 890 °C to investigate through short disequilibrium and long near equilibrium experiments the influence of diffusive re-equilibration on trace element partitioning during crystallization. Our data show that Ba and Sr behave compatibly, and their partition coefficients are influenced by re-equilibration time, orthoclase (Or) content, growth rate and cation order-disorder. High field strength elements (HFSE) and rare earth elements (except Eu) are strongly incompatible, but alkali feldspar efficiently fractionates light (LREE) from heavy rare earth elements (HREE). Our crystallization experiments reveal a strong influence of disequilibrium crystal growth on the partitioning of Ba and Sr. In particular, short-duration experiments show that rapid alkali feldspar crystal growth after nucleation, promotes disordered growth and less selectivity in the partitioning of compatible trace elements that easily enter the crystal lattice (e.g., Ba and Sr)....

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Fabio Arzilli, Alessandro Fabbrizio, M. W. Schmidt, Maurizio Petrelli, M Maimaiti, D. B. Dingwell, E. Paris, M. Burton, M. Carroll. 2018-12-26. The effect of diffusive re-equilibration time on trace element partitioning between alkali feldspar and trachytic melts. https://doi.org/10.1016/j.chemgeo.2018.07.035

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