Abstract: In Situ Monitoring of Microstructures during Subsequent Phase Transitions in the Olivine System up to 30 GPa and 1100 K Using 3D-XRD Single-Grain Analysis. Effects of Grain Size Evolution on the Stagnation of Slab. (2014 AGU Fall Meeting)

In Situ Monitoring of Microstructures during Subsequent Phase Transitions in the Olivine System up to 30 GPa and 1100 K Using 3D-XRD Single-Grain Analysis. Effects of Grain Size Evolution on the Stagnation of Slab.

Angelika Rosa¹, Nadege Hilairet¹, Dr. Sujoy Ghosh, PhD², Jeroen Jacobs³, Jean-Philippe Perrillat⁴, Gavin B.M, Vaughan³, Gaston Garbarino³, Nohamed Mezouar³ and Sebastien Merkel⁵, (1)University of Lille 1, Villeneuve d'Ascq, France, (2)ETH Swiss Federal Institute of Technology Zurich, Zurich, Switzerland, (3)ESRF European Synchrotron Radiation Facility, Grenoble, France, (4)Laboratoire de Géologie de Lyon - Université Claude Bernard Lyon1, Villeurbanne, France, (5)UMET, Université de Lille, Villeneuve d'Ascq, France

Abstract:

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