Interplay between seismic fracture and aseismic creep in the Woodroffe Thrust, central Australia – Inferences for the rheology of relatively dry continental mid-crustal levels
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DOI: 10.1016/j.tecto.2018.10.024
Abstract: Abstract The over 600 km long Woodroffe Thrust developed at lower to mid-crustal levels during the intracontinental Petermann Orogeny at ca. 560–520 Ma. Ductile deformation with a top-to-north shear sense was accommodated along a shallowly (≤30°) south-dipping… read more here.
Keywords: crustal levels; rheology; mid crustal; woodroffe thrust ... See more keywords