| Reference Type | Journal (article/letter/editorial) |
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| Title | Late Quaternary movement of Aspy Fault, Nova Scotia |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Grant, Douglas R. | Author |
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| Year | 1990 (July 1) | Volume | 27 |
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| Issue | 7 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e90-100Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 480970 | Long-form Identifier | mindat:1:5:480970:2 |
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| GUID | 0 |
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| Full Reference | Grant, Douglas R. (1990) Late Quaternary movement of Aspy Fault, Nova Scotia. Canadian Journal of Earth Sciences, 27 (7) 984-987 doi:10.1139/e90-100 |
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| Plain Text | Grant, Douglas R. (1990) Late Quaternary movement of Aspy Fault, Nova Scotia. Canadian Journal of Earth Sciences, 27 (7) 984-987 doi:10.1139/e90-100 |
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| In | (1990, July) Canadian Journal of Earth Sciences Vol. 27 (7) Canadian Science Publishing |
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| Abstract/Notes | An emerged Sangamonian (125 ka) intertidal rock platform at +7 m asl is apparently upthrown to +22 m asl along Aspy Fault on Cape Breton Island. The 15 m displacement may be an isostatic response to rapid ice retreat or erosional unloading, or it may be a tectonic effect due to release of crustal stress stored during Wisconsinan glacier cover. |
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