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Experimental constraints on majorite stability in the Earth's interior

Subject Area Mineralogy, Petrology and Geochemistry
Term from 2009 to 2014
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 154174661
 
Final Report Year 2016

Final Report Abstract

The main aim of this study was to experimentally investigate the stability of majorite garnets in depleted mantle compositions and to develop a new geobarometer for majorite garnets. To address these objectives we addressed the aforementioned issues: We successfully performed high-pressure experiments and some additional calibration runs in the Münster multi anvil apparatus, we investigated the stability of majorite garnets at different pressures, temperatures, and chemical compositions, and developed a new geobarometer that links chemical composition of majoritic garnet with pressure. The experimental results together with the new geobarometer will enable refined geobarometry of majoritic garnets found as inclusions in diamonds or in high-pressure rocks. As we experienced a major breakdown of our multi anvil apparatus, during which it was not operational for more than six months, we also conducted two minor experimental studies in depleted bulk compositions at atmospheric pressure. The first study focussed on the effects of Cr on trace element partitioning between spinel and silicate melts. In the other minor project we measured new thermodynamic properties of the Cr-endmember garnet knorringite.

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