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Stability of melt-rich channels in Earth’s mantle  High Pressure and Temperature Experiments of Olivine, Chromite and Mid-Ocean Ridge Basalt (MORB) Kristyn Rodzinyak Dan King,  PhD student,  Rock and Mineral Physics Lab, Department of Geology and Geophysics, University of Minnesota, Minneapolis Mark Zimmerman, UMN David Kohlstedt, UMN
Melt  Transport ,[object Object],http://www.yorku.ca/esse/veo/earth/image/1-3-2. JPG
Stress Driven Melt Segregation ,[object Object],[object Object],http://www.waterencyclopedia.com/images/wsci_03_img0352.jpg http://sio.ucsd.edu/volcano/about/images/recycle.gif http://visearth.ucsd.edu/VisE_Int/platetectonics/hotspot2.jpg ,[object Object]
Samples ,[object Object],[object Object],[object Object],Torsion   Static Anneal
Sample Preparation Deformation Assembly
Experiments Gas-medium deformation apparatus PI-10 300 MPa ~10 Km depth  Torsion Actuator   Pressure Vessel   Leak Detector   Thermocouple
Torsion, 1473K, 300 MPA Data during first deformation. A slow leak (1MPa/ 6 mins) caused the termination of the experiment. Torsion, 1473K, 200MPa Second deformation on sample once rejacketed.  Run terminated due to a slip along a boundary indicated by a drastic drop in plots.
Melt-Rich Bands 1000µm No Bands Bands Bands
Results-Torsion Distance (microns) 20 µm
Results-Static Anneal Distance (microns) 20 µm
Scanning Electron Microscope   2 µm
Quenched   1 hour anneal  10 hour anneal
Conclusions  ,[object Object],[object Object],[object Object],[object Object]
David Kohlstedt’s Rock and Mineral Physics Lab
Special Thanks To… ,[object Object],[object Object]

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Stability of Melt Rich Channels