| Reference Type | Journal (article/letter/editorial) |
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| Title | Polished and Striated Mud Surfaces in the St. Lawrence Tidal Flats, Quebec |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Dionne, Jean-Claude | Author |
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| Year | 1974 (June 1) | Volume | 11 |
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| Issue | 6 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e74-086Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 474134 | Long-form Identifier | mindat:1:5:474134:7 |
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| GUID | 0 |
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| Full Reference | Dionne, Jean-Claude (1974) Polished and Striated Mud Surfaces in the St. Lawrence Tidal Flats, Quebec. Canadian Journal of Earth Sciences, 11 (6) 860-866 doi:10.1139/e74-086 |
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| Plain Text | Dionne, Jean-Claude (1974) Polished and Striated Mud Surfaces in the St. Lawrence Tidal Flats, Quebec. Canadian Journal of Earth Sciences, 11 (6) 860-866 doi:10.1139/e74-086 |
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| In | (1974, June) Canadian Journal of Earth Sciences Vol. 11 (6) Canadian Science Publishing |
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| Abstract/Notes | Drift ice polishes and striates the surface of mud tidal flats along the St. Lawrence Estuary. Drag marks are due to tidal currents dragging ice cakes on the bottom. Striated and polished mud surfaces can be fossilized and preserved. If found in consolidated sedimentary rocks, they would be indicators of: the top of a bed, current direction, shallow water, and a cold environment. |
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