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KINEMATICS AND VORTICITY IN KANGMAR DOME, SOUTHERN TIBET:TESTING MIDCRUSTAL CHANNEL FLOW MODELS FOR THE HIMALAYA (2010)
This paper is about the kinematic, kinematic vorticity (Wm), and deformation temperature analyses that were completed to test the hypothesis that midcrustal rocks exposed in the core of the Kangmar gneiss dome, southern Tibet record ductile deformation patterns of a �frozen� segment of a southward flowing midcrustal channel.
Reference:
TECTONICS, VOL. 29, TC6011, doi:10.1029/2010TC002746, 2010
TECTONICS, VOL. 29, TC6011, doi:10.1029/2010TC002746, 2010
Organization:
Department of Geological Sciences, Central Washington University, Ellensburg, Washington, USA
Tibet
Department of Geological Sciences, Central Washington University, Ellensburg, Washington, USA
Tibet
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