Thermal Structure of Mid-Crustal Shear Zones
Analysis of quartz c-axis fabrics and microstructures from ductily deformed rocks allows for the examination of the kinematics associated with crustal deformation. This thesis expands on the current knowledge of the kinematic evolution of the Himalayas and Scottish Caledonides, by examining samples...
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Virginia Tech
2013
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| Online Access: | http://hdl.handle.net/10919/23284 |