| Reference Type | Journal (article/letter/editorial) |
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| Title | Intra-Stratal Flow and Convolute Folding |
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| Journal | Geological Magazine |
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| Authors | Williams, Emyr | Author |
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| Year | 1960 (June) | Volume | 97 |
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| Issue | 3 |
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| Publisher | Cambridge University Press (CUP) |
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| DOI | doi:10.1017/s0016756800061380 |
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| Generate Citation Formats |
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| Mindat Ref. ID | 248965 | Long-form Identifier | mindat:1:5:248965:4 |
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| GUID | 0 |
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| Full Reference | Williams, Emyr (1960) Intra-Stratal Flow and Convolute Folding. Geological Magazine, 97 (3) 208-214 doi:10.1017/s0016756800061380 |
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| Plain Text | Williams, Emyr (1960) Intra-Stratal Flow and Convolute Folding. Geological Magazine, 97 (3) 208-214 doi:10.1017/s0016756800061380 |
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| In | (1960, June) Geological Magazine Vol. 97 (3) Cambridge University Press (CUP) |
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| Abstract/Notes | AbstractThe property of liquefaction of certain confined, water-logged, unconsolidated sedimentary layers is considered to play an important part in the development of much of convolute folding. Lateral intrastratal laminar flow of liquefied beds, according to flow patterns mainly determined by the distribution of parts of the layers that have remained solid, appears to account satisfactorily for internal folding. Although intra-stratal flow, which can result from a number of causes, may considerably deform the stratification planes of a liquefied layer, there is neither lateral shortening nor a notable change in the thickness of the bed. |
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