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Madi Fleming
University of OtagoMeeting roles in:
Fabric-Induced Weakening of Ice During Tertiary Creep at High Shear Strain
Effects of Shear-Driven Crystallographic Preferred Orientation on the Compressional Flow Stress of Ice
Microstructural evolution of ice in a laterally-confined, plane-strain geometry
The evolution of crystallographic preferred orientations in ice under changing deformation kinematics
Infiltration Instabilities in Partially Molten Ice
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