Implications of thrust and detachment faulting for the structural geology of the Thermo Hot Springs KGRA, Utah (OFR-587) UGA MP Sedimentary structures

Sedimentary structures

Central African Republic

which adds up to a ton of local knowledge

Pine Hollow

shaded relief

Implications of thrust and detachment faulting for the structural geology of the Thermo Hot Springs KGRA, Utah (OFR-587) UGA MP Sedimentary structuresBy: W. Anderson and R. L. Bruhn The Sevier geothermal anomaly of southwestern Utah encompasses a broad region of enhanced heat flow with seven known high temperature geothermal resource areas or "KGRA". The anomaly also encompasses the transition between the Colorado Plateau and the eastern Basin and Range Province, where the Paleozoic miogeocline was collapsed eastward by thrust faulting during the Cretaceous to early Tertiary Sevier orogeny, which