Late Cretaceous Tectonic Evolution Of The Deep Creek-Kern Mountains, Eastern Nevada And Western Utah: Magmatically Induced Large-Scale Folding, Dynamothermal Metamorphism And Ductile Strain At Mid- To Upper-Crustal Levels In The Sevier Hinterland
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Late Cretaceous Tectonic Evolution Of The Deep Creek-Kern Mountains, Eastern Nevada And Western Utah: Magmatically Induced Large-Scale Folding, Dynamothermal Metamorphism And Ductile Strain At Mid- To Upper-Crustal Levels In The Sevier Hinterland