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Implications of thrust and detachment faulting for the structural geology of the Thermo Hot Springs KGRA, Utah (OFR-587) UGA MP shaded relief
Implications of thrust and detachment faulting for the structural geology of the Thermo Hot Springs KGRA, Utah (OFR-587) UGA MP shaded relief
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shaded relief
Central African Republic
Sedimentary structures
By: Richard A
Implications of thrust and detachment faulting for the structural geology of the Thermo Hot Springs KGRA, Utah (OFR-587) UGA MP shaded reliefBy: 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
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