| Reference Type | Journal (article/letter/editorial) |
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| Title | A newly recognized sequence of possible Early Cambrian age in southern New Brunswick: evidence for major southward-directed thrusting |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | McLeod, M. J. | Author |
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| McCutcheon, S. R. | Author |
| Year | 1981 (June 1) | Volume | 18 |
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| Issue | 6 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e81-097Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 477129 | Long-form Identifier | mindat:1:5:477129:0 |
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| GUID | 0 |
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| Full Reference | McLeod, M. J., McCutcheon, S. R. (1981) A newly recognized sequence of possible Early Cambrian age in southern New Brunswick: evidence for major southward-directed thrusting. Canadian Journal of Earth Sciences, 18 (6) 1012-1017 doi:10.1139/e81-097 |
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| Plain Text | McLeod, M. J., McCutcheon, S. R. (1981) A newly recognized sequence of possible Early Cambrian age in southern New Brunswick: evidence for major southward-directed thrusting. Canadian Journal of Earth Sciences, 18 (6) 1012-1017 doi:10.1139/e81-097 |
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| In | (1981, June) Canadian Journal of Earth Sciences Vol. 18 (6) Canadian Science Publishing |
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| Abstract/Notes | Several previously unidentified occurrences of possible Lower Cambrian strata have been discovered recently in the Eastern Volcanic Belt (Avalon zone) of southern New Brunswick. The basal part of the sequence is lithologically similar to the Lower Cambrian parastratotype on Hanford Brook near Saint John, New Brunswick. Some of the newly recognized Cambrian rocks crop out beneath major northeast-trending and north-dipping thrusts, and rest unconformably on subaqueous Upper Precambrian equivalents of the Coldbrook Group. The presence of these Cambrian rocks in the Eastern Volcanic Belt indicates that the Cambrian–Ordovician Iapetus Ocean transgressed across the entire Avalon zone of southern New Brunswick. |
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These are possibly similar items as determined by title/reference text matching only.
