A Two-Stage Model for Extension in the Northern Rio Grande Rift: From Localized Ductile Shear Coeval with Magmatism to Regional-Scale Brittle Faulting and Exhumation
A Two-Stage Model for Extension in the Northern Rio Grande Rift: From Localized Ductile Shear Coeval with Magmatism to Regional-Scale Brittle Faulting and Exhumation