| Reference Type | Journal (article/letter/editorial) |
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| Title | On the position of the Variscan front in southern New Brunswick and its relation to Precambrian basement |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Rast, N. | Author |
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| Currie, K. L. | Author |
| Year | 1976 (January 1) | Volume | 13 |
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| Issue | 1 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e76-021Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 474676 | Long-form Identifier | mindat:1:5:474676:2 |
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| GUID | 0 |
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| Full Reference | Rast, N., Currie, K. L. (1976) On the position of the Variscan front in southern New Brunswick and its relation to Precambrian basement. Canadian Journal of Earth Sciences, 13 (1) 194-196 doi:10.1139/e76-021 |
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| Plain Text | Rast, N., Currie, K. L. (1976) On the position of the Variscan front in southern New Brunswick and its relation to Precambrian basement. Canadian Journal of Earth Sciences, 13 (1) 194-196 doi:10.1139/e76-021 |
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| In | (1976, January) Canadian Journal of Earth Sciences Vol. 13 (1) Canadian Science Publishing |
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| Abstract/Notes | The Variscan front is marked by a zone of cataclasis that generally follows an older and larger mylonite zone, but locally cuts across relatively undeformed Precambrian rocks. The older mylonite zone probably developed in Late Precambrian (Avalonian) time. Correlative Precambrian rocks extend across both the Variscan front, and the Bellisle fault to the northwest. |
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These are possibly similar items as determined by title/reference text matching only.
