Transport and storage of incompatible trace elements in phosphorus enriched peridotitic mantle
Published: 18 May 2026| Version 1 | DOI: 10.17632/3tzdkh2rbf.1
Contributor:
Tristan PauschDescription
SIMS analyses of trace element contents in all coexisting phases (bridgmanite, clinoenstatite, davemaoite, ferropericlase, forsterite, garnet, quenched liquid, ringwoodite, tuite and wadsleyite) in a phosphorus enriched peridotite at upper to lower mantle transition zone conditions. Experiments were performed in a P-T range of 15-25 GPa and between 1600 and 1800°C.
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Institutions
- Universität InnsbruckTyrol, Innsbruck
Categories
Earth Sciences, Mineralogy, Experimental Petrology