| Reference Type | Journal (article/letter/editorial) |
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| Title | Geothermal gradients in the Hinton area of west-central Alberta |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Lam, H. L. | Author |
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| Jones, F. W. | Author |
| Lambert, C. | Author |
| Year | 1982 (April 1) | Volume | 19 |
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| Issue | 4 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e82-064Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 477448 | Long-form Identifier | mindat:1:5:477448:2 |
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| GUID | 0 |
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| Full Reference | Lam, H. L., Jones, F. W., Lambert, C. (1982) Geothermal gradients in the Hinton area of west-central Alberta. Canadian Journal of Earth Sciences, 19 (4) 755-766 doi:10.1139/e82-064 |
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| Plain Text | Lam, H. L., Jones, F. W., Lambert, C. (1982) Geothermal gradients in the Hinton area of west-central Alberta. Canadian Journal of Earth Sciences, 19 (4) 755-766 doi:10.1139/e82-064 |
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| In | (1982, April) Canadian Journal of Earth Sciences Vol. 19 (4) Canadian Science Publishing |
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| Abstract/Notes | Temperature data from petroleum exploration well logs of 3360 wells in a region of west-central Alberta are used to estimate thermal gradients. A relatively high geothermal gradient (~36 °C/km) of oblong shape located near Hinton is observed. The axis of the anomaly strikes approximately southwest–northeast and passes through the Miette Hot Springs area. It appears that water is heated at depth in the Rocky Mountain disturbed region and travels eastward and toward the surface along fault planes. |
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