| Reference Type | Journal (article/letter/editorial) |
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| Title | New Light on Sedimentation and Tectonics |
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| Journal | Geological Magazine |
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| Authors | Bailey, E. B. | Author |
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| Year | 1930 (February) | Volume | 67 |
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| Page(s) | 77-92 | Issue | 2 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800098927 |
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| Mindat Ref. ID | 245775 | Long-form Identifier | mindat:1:5:245775:2 |
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| GUID | 7ae6edee-9669-43e6-9761-8de4dac7293a |
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| Full Reference | Bailey, E. B. (1930) New Light on Sedimentation and Tectonics. Geological Magazine, 67 (2) 77-92 doi:10.1017/s0016756800098927 |
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| Plain Text | Bailey, E. B. (1930) New Light on Sedimentation and Tectonics. Geological Magazine, 67 (2) 77-92 doi:10.1017/s0016756800098927 |
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| In | (1930, February) Geological Magazine Vol. 67 (2) Cambridge University Press (CUP) |
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| Abstract/Notes | 1. The Loch Awe Nappe succession was correctly stated in 1922.2. The Iltay Nappe succession was correctly stated in 1922.3. The Ballappel Foundation succession was wrongly stated in 1922.4. The recumbent-fold structure of the Ballachulish district is due to rotation of middle limbs by drag from above or from below.5. Graded bedding is as important as current bedding in marking a facies group among sandstones. It often indicates accumulation in rather deep water, to which sandy material has penetrated, perhaps as a result of seaquakes. |
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