| Reference Type | Journal (article/letter/editorial) |
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| Title | The Deformation of Confined, Incompetent Layers in Folding |
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| Journal | Geological Magazine |
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| Authors | Williams, Emyr | Author |
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| Year | 1961 (August) | Volume | 98 |
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| Issue | 4 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800060647Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 249087 | Long-form Identifier | mindat:1:5:249087:2 |
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| GUID | 0 |
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| Full Reference | Williams, Emyr (1961) The Deformation of Confined, Incompetent Layers in Folding. Geological Magazine, 98 (4) 317-323 doi:10.1017/s0016756800060647 |
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| Plain Text | Williams, Emyr (1961) The Deformation of Confined, Incompetent Layers in Folding. Geological Magazine, 98 (4) 317-323 doi:10.1017/s0016756800060647 |
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| In | (1961, August) Geological Magazine Vol. 98 (4) Cambridge University Press (CUP) |
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| Abstract/Notes | AbstractShearing stresses acting on an incompetent layer confined between competent beds during its deformation in the development of folds, differ from those commonly accepted as the cause of a number of minor structures associated with the deformation. It is suggested that the effect of bedding drag is negligible, and that the structures described as slaty cleavage, fracture cleavage, and drag folds can be explained by the laminar flow of the incompetent material whilst accommodating itself to the interspaces determined by the more competent layers. |
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