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Drury, Malcolm, Taylor, Alan (1987) Some new measurements of heat flow in the Superior Province of the Canadian Shield. Canadian Journal of Earth Sciences, 24 (7) 1486-1489 doi:10.1139/e87-140

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Reference TypeJournal (article/letter/editorial)
TitleSome new measurements of heat flow in the Superior Province of the Canadian Shield
JournalCanadian Journal of Earth Sciences
AuthorsDrury, MalcolmAuthor
Taylor, AlanAuthor
Year1987 (July 1)Volume24
Page(s)1486-1489Issue7
PublisherCanadian Science Publishing
DOIdoi:10.1139/e87-140Search in ResearchGate
Mindat Ref. ID479641Long-form Identifiermindat:1:5:479641:5
GUID5aa65637-7244-49a5-92c0-1d3d88706616
Full ReferenceDrury, Malcolm, Taylor, Alan (1987) Some new measurements of heat flow in the Superior Province of the Canadian Shield. Canadian Journal of Earth Sciences, 24 (7) 1486-1489 doi:10.1139/e87-140
Plain TextDrury, Malcolm, Taylor, Alan (1987) Some new measurements of heat flow in the Superior Province of the Canadian Shield. Canadian Journal of Earth Sciences, 24 (7) 1486-1489 doi:10.1139/e87-140
In(1987, July) Canadian Journal of Earth Sciences Vol. 24 (7) Canadian Science Publishing
Abstract/Notes Borehole heat-flow measurements are reported from six new sites in the Superior Province of the Canadian Shield. Values adjusted for glaciation effects, but not for Holocene climatic variations, range from 42 to 56 mW/m2. When these new values are combined with 21 previously published borehole values the mean is 42 mW/m2 with a standard deviation of 11 mW/m2. The data for a site on the Lac du Bonnet batholith suggest that the batholith has a thin veneer, less than 3 km, of rock of high radiogenic heat production at the surface.


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