| Reference Type | Journal (article/letter/editorial) |
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| Title | Mylonite, Slickensides, and the Great Glen Fault |
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| Journal | Geological Magazine |
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| Authors | Shand, S. J. | Author |
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| Year | 1951 (December) | Volume | 88 |
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| Issue | 6 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800069971 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 248105 | Long-form Identifier | mindat:1:5:248105:4 |
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| GUID | 0 |
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| Full Reference | Shand, S. J. (1951) Mylonite, Slickensides, and the Great Glen Fault. Geological Magazine, 88 (6) 423-428 doi:10.1017/s0016756800069971 |
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| Plain Text | Shand, S. J. (1951) Mylonite, Slickensides, and the Great Glen Fault. Geological Magazine, 88 (6) 423-428 doi:10.1017/s0016756800069971 |
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| In | (1951, December) Geological Magazine Vol. 88 (6) Cambridge University Press (CUP) |
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| Abstract/Notes | AbstractIt is shown that mylonite is extremely rare in the plane of the Great Glen fault, and that horizontal slickensides or friction-grooves directed along the Glen are virtually absent. Grave doubt is consequently thrown on the alleged horizontal displacement in the fault zone. |
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These are possibly similar items as determined by title/reference text matching only.
