| Reference Type | Journal (article/letter/editorial) |
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| Title | Analysis of Heat-Flow Data—Several Boreholes in a Sedimentary Basin |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Judge, A. S. | Author |
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| Beck, A. E. | Author |
| Year | 1973 (October 1) | Volume | 10 |
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| Issue | 10 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e73-142Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 473514 | Long-form Identifier | mindat:1:5:473514:8 |
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| GUID | 0 |
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| Full Reference | Judge, A. S., Beck, A. E. (1973) Analysis of Heat-Flow Data—Several Boreholes in a Sedimentary Basin. Canadian Journal of Earth Sciences, 10 (10) 1494-1507 doi:10.1139/e73-142 |
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| Plain Text | Judge, A. S., Beck, A. E. (1973) Analysis of Heat-Flow Data—Several Boreholes in a Sedimentary Basin. Canadian Journal of Earth Sciences, 10 (10) 1494-1507 doi:10.1139/e73-142 |
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| In | (1973, October) Canadian Journal of Earth Sciences Vol. 10 (10) Canadian Science Publishing |
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| Abstract/Notes | For the Western Ontario and Michigan basins, which overlie the Grenville and Central geological provinces, temperature gradients in more than 30 boreholes and thermal conductivities of several hundred specimens from several formations have been determined. It is found that characteristic gradients and conductivities can be assigned to certain formations and to geological periods. There may also be a real variation (< 20%) of heat flow between some formations, which is qualitatively correlated with variations in heat producing elements.With the exception of one value of 1.3 μcal cm−2 s−1, which involved extrapolation of data to a great distance, all 'whole borehole' heat-flow values, uncorrected for glaciation effects, lie between 1.0 ± 0.2 μcal cm−2 s−1; a correction for the Wisconsin stage of the Pleistocene glaciation would increase these values by 0.3 ± 0.1 μcal cm−2 s−1. |
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