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- W2129134051 abstract "Forty-one measurements of heat flow, including three close-spaced groups of measurements, were taken at positions extending from the continental slope off Oregon to the east flank of the Juan de Fuca ridge. Individual values ranged from 1.08 μcal/cm2 sec in 445 meters of water on the continental slope off Oregon to 7.21 μcal/cm2 sec measured in 2740 meters of water near the Juan de Fuca ridge crest. The mean of the 41 heat-flow values is 2.86 μcal/cm2 sec, which is considerably higher than the approximate global mean of 1.5 μcal/cm2 sec. This high average heat flow fits the previously deduced world heat-flow pattern, which includes a high over the eastern Pacific. The distribution of 16 heat-flow measurements taken from near the base of the continental slope off Oregon westward to Cascadia channel has a broad peak between 1.50 and 2.99 μcal/cm2 sec. The distribution of 15 heat-flow measurements taken from west of Cascadia channel to near the Juan de Fuca ridge crest has a relatively sharp peak between 3.50 and 3.99 μcal/cm2 sec. The results of this research, combined with existing heat-flow data for the west flank of the Juan de Fuca ridge, show that the heat-flow profile across this ridge is not symmetrical. Unusually low values predominate on the west-flank, whereas above average values dominate the east flank of the Juan de Fuca ridge." @default.
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- W2129134051 date "1971-07-10" @default.
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- W2129134051 title "Heat flow through the floor of Cascadia Basin" @default.
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- W2129134051 doi "https://doi.org/10.1029/jb076i020p04758" @default.
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