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Gravity and thermal models of the twin peaks magma system, West-Central Utah

Conference · · Trans. - Geotherm. Resour. Counc.; (United States)
OSTI ID:6375277
Gravity, heat flow, surface geology, and geochemistry have been integrated to evaluate the geothermal potential of a site of late Tertiary silicic volcanism at Twin Peaks, Utah. Volcanism began in the area with the extrusion of the Coyote Hills rhyolite 2.74+-.1 m.y. ago, and was resumed, after .2 m.y. of quiescence, with the extrusion of a complex sequence of domes and flows that lasted until 2.35+-.07 m.y. ago. Residual gravity in the Twin Peaks area is characterized by a roughly circular and broad 7 mgal gravity low possibly related to a body intruding the basement. The intrusion can be approximated by a three-dimensional vertical cylinder with a roof at the depth of 3 km, a radius about 6 km, and a thickness of 2.25 - 3.5 km. Simple conductive thermal models predict a maximum anomalous heat flow of 175 mW/m/sup 2/ at surface, 90,000 years after emplacement of the intrusion. Model prediction of negligible residual heat flow at the present is consistent with measured heat flow of 96 mW/m/sup 2/ at Twin Peaks, which is indistinguishable from background Basin and Range heat flow.
OSTI ID:
6375277
Report Number(s):
CONF-800920-
Conference Information:
Journal Name: Trans. - Geotherm. Resour. Counc.; (United States) Journal Volume: 4
Country of Publication:
United States
Language:
English