Geodynamics of Cenozoic extension along a transect across the Colorado River extensional corridor, southwestern USA
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DOI: 10.1130/l1002.1
Abstract: The Colorado River extensional corridor in southwestern North America is one of Earth’s most highly extended regions of continental crust. The central part of the belt includes three imbricate, regionally northeast-dipping extensional detachment faults. The… read more here.
Keywords: fault; plomosa detachment; detachment fault; detachment ... See more keywords