| Reference Type | Journal (article/letter/editorial) |
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| Title | An Analysis of the Deformation in a Fold in North-east Tasmania |
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| Journal | Geological Magazine |
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| Authors | Williams, Emyr | Author |
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| Year | 1966 (April) | Volume | 103 |
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| Issue | 2 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800050494Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 249607 | Long-form Identifier | mindat:1:5:249607:2 |
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| GUID | 0 |
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| Full Reference | Williams, Emyr (1966) An Analysis of the Deformation in a Fold in North-east Tasmania. Geological Magazine, 103 (2) 115-119 doi:10.1017/s0016756800050494 |
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| Plain Text | Williams, Emyr (1966) An Analysis of the Deformation in a Fold in North-east Tasmania. Geological Magazine, 103 (2) 115-119 doi:10.1017/s0016756800050494 |
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| In | (1966, April) Geological Magazine Vol. 103 (2) Cambridge University Press (CUP) |
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| Abstract/Notes | AbstractMicroscope studies of a flattened fold are consistent with conclusions from macroscopic observations that whereas mudstone cleavage development may have resulted from a laminar-type flow governed by competent confining sandstone beds, the sandstone cleavage appears to be related to the dilation of texture during the early stages of deformation. Continued deformation results in a textural disruption of the initially competent sandstone, which is considered to allow flattening. |
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