| Reference Type | Journal (article/letter/editorial) |
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| Title | Paleomagnetism of the Sutton Lake Proterozoic inlier, Ontario, Canada |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Schwarz, E. J. | Author |
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| Clark, K. R. | Author |
| Fujiwara, Y. | Author |
| Year | 1982 (June 1) | Volume | 19 |
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| Issue | 6 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e82-114Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 477551 | Long-form Identifier | mindat:1:5:477551:9 |
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| GUID | 0 |
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| Full Reference | Schwarz, E. J., Clark, K. R., Fujiwara, Y. (1982) Paleomagnetism of the Sutton Lake Proterozoic inlier, Ontario, Canada. Canadian Journal of Earth Sciences, 19 (6) 1330-1332 doi:10.1139/e82-114 |
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| Plain Text | Schwarz, E. J., Clark, K. R., Fujiwara, Y. (1982) Paleomagnetism of the Sutton Lake Proterozoic inlier, Ontario, Canada. Canadian Journal of Earth Sciences, 19 (6) 1330-1332 doi:10.1139/e82-114 |
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| In | (1982, June) Canadian Journal of Earth Sciences Vol. 19 (6) Canadian Science Publishing |
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| Abstract/Notes | Thirty-eight cores were collected from eight sites in the Sutton Lake Proterozoic inlier, which is thought to be an extension of the Circum-Ungava Belt. Six sites from a 100 m thick diabase sill yielded essentially single-component magnetization averaging D = 35°, I = −54°, k = 39,α95 = 11°. The diabase dips north at 4° and shows only minor alteration (epidote and chlorite). The other two sites were in a fine-grained dark layer within the sill and in a dike. No end points were observed for these sites upon alternating field and thermal demagnetization. The six diabase sites yielded a north pole at 67°E, 3°S, dm = 15, dp = 11. This pole position is similar to that obtained for the youngest volcanic suite (Flaherty Formation) of the Belcher Islands and to that obtained for red beds of the La Grande 4 outlier, suggesting a time-stratigraphic correlation between these units. |
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