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- W1992151454 abstract "Eight holes in southwestern Virginia provided a heat flow value at Cripple Creek (36°49′N, 81°06′W) of 1.03 ± 0.15 μcal/cm2 sec and a value of 1.7 ± 0.34 μcal/cm2 sec near Grundy (37°20′N, 82°W). The value of 1.03 μcal/cm2 sec agrees with low values to the northeast reported by Diment. The possibility of low heat flow due to nonequilibrium gradients resulting from late Paleozoic overthrusting was investigated. It was concluded that any reasonable model would be close to equilibrium in less than 80 m.y. The low heat flow value at Cripple Creek is probably the result of erosion of the upper crust before deposition of late Precambrian and Paleozoic sediments. Heat production studies of surface rocks near Alberta, Virginia, support the high heat flow of 1.4 μcal/cm2 sec obtained there by Diment and Werre (1964)." @default.
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- W1992151454 date "1973-03-10" @default.
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- W1992151454 title "Heat flow in southwestern Virginia" @default.
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- W1992151454 doi "https://doi.org/10.1029/jb078i008p01323" @default.
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