Stability of Majorite garnet in the deep Earth

Basic data of the doctoral examination procedure

Doctoral examination procedure finished at: Doctoral examination procedure at University of Münster

Period of time: 01/10/2011 - 27/11/2015

Status: completed

Candidate: Wijbrans, Clazina

Doctoral subject: Mineralogie

Doctoral degree: Dr. rer. nat.

Awarded by: Department 14 - Geosciences

Supervisors: Klemme, Stephan

Institute for Mineralogy

Professur für Petrologie (Prof. Klemme)

Duration: 17/07/2009 - 31/12/2015

Funded by: DFG - Individual Grants Programme

Type of project: Individual project

An experimental investigation of the stability of majoritic garnet in the Earth’s mantle and an improved majorite geobarometer Wijbrans CH, Rohrbach A, Klemme S (2016) In: Contributions to Mineralogy and Petrology, 171(50). Research article (journal)
The Stability of Majoritic Garnet Depending on Garnet Composition Wijbrans CH, Rohrbach A, Klemme S (2015) In: (eds.), . (kein Verlag angegeben). Research article in edited proceedings (conference)
Experimental determination of trace element partition coefficients between spinel and silicate melt: The influence of chemical composition and oxygen fugacity Wijbrans CH, Klemme S, Berndt J, Vollmer C (2015) In: Contributions to Mineralogy and Petrology, 69(4). Research article (journal)
The stability of Fe-Ni carbides in the Earth's mantle: Evidence for a low Fe-Ni-C melt fraction in the deep mantle Rohrbach A, Ghosh S, Schmidt MW, Wijbrans CH, Klemme S (2014) In: Earth and Planetary Science Letters, 388. Research article (journal)
Thermodynamic and magnetic properties of knorringite garnet (Mg3Cr2Si3O12) based on low-temperature calorimetry and magnetic susceptibility measurements Wijbrans CH, Niehaus O, Rohrbach A, Pöttgen R, Klemme S (2014) In: Physics and Chemistry of Minerals, 41. Research article (journal)