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Regional trends in radiogenic heat generation in the Precambrian basement of the Western Canadian Basin
Author(s) -
Jones F. W.,
Majorowicz J. A.
Publication year - 1987
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/gl014i003p00268
Subject(s) - radiogenic nuclide , precambrian , geology , heat generation , basement , paleozoic , crust , geochemistry , geomorphology , petrology , mantle (geology) , physics , civil engineering , engineering , thermodynamics
Radiogenic heat generation values for 381 basement samples from 229 sites in the western Canadian basin exhibit a lognormal frequency distribution. The mean value = 2.06 (S.D. = 1.22) µWm −3 is larger than the radiogenic heat generation values reported for the shield in the Superior (ca. 1.2 µWm −3 , Jessop and Lewis, 1978) and Churchill (ca. 0.7 µWm −3 , Drury, 1985) provinces. When equal Log A contour intervals are used to map the basement heat generation, three large zones of relatively high heat generation are found. One coincides with the Peace River Arch basement structure and one with the Athabasca axis (Darnley, 1981). There is no apparent indication of increased heat flow through the Paleozoic formations associated with these two zones. The third zone, in southwestern Saskatchewan, coincides with a high heat flow zone in the Swift Current area. The lack of correlation between heat flow and heat generation in Alberta may be due to the disturbance to the heat flow in the Paleozoic formations by water motion, or may indicate that the heat is from uranium, thorium and potassium isotope enrichment near the basement surface rather than enrichment throughout the entire upper crust.