Reference Type | Journal (article/letter/editorial) |
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Title | Textural responses to evolving mass-flows: an example from the Devonian Asen Formation, central Norway |
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Journal | Geological Magazine |
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Authors | Bøe, Reidulv | Author |
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Sturt, Brian A. | Author |
Year | 1991 (March) | Volume | 128 |
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Issue | 2 |
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Publisher | Cambridge University Press (CUP) |
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DOI | doi:10.1017/s0016756800018306Search in ResearchGate |
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| Generate Citation Formats |
Mindat Ref. ID | 254966 | Long-form Identifier | mindat:1:5:254966:2 |
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GUID | 0 |
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Full Reference | Bøe, Reidulv, Sturt, Brian A. (1991) Textural responses to evolving mass-flows: an example from the Devonian Asen Formation, central Norway. Geological Magazine, 128 (2) 99-109 doi:10.1017/s0016756800018306 |
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Plain Text | Bøe, Reidulv, Sturt, Brian A. (1991) Textural responses to evolving mass-flows: an example from the Devonian Asen Formation, central Norway. Geological Magazine, 128 (2) 99-109 doi:10.1017/s0016756800018306 |
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In | (1991, March) Geological Magazine Vol. 128 (2) Cambridge University Press (CUP) |
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Abstract/Notes | AbstractThe Asenvågoya Conglomerate is a thin (c. 6 m) conglomeratic body composed of mass-flow deposits and enveloped by braided-stream sandstones and conglomerates. The section studied represents the proximal part of a small-radius alluvial fan built out from the basin margin towards a flood basin. The fan was possibly generated by escarpment creation, or rejuvenation, in response to syndepositional faulting along the basin margin, and comprises sand-matrix-supported and clast-supported, sheet-like conglomerates. There is an upward change through the sequence from stream flow and surging mass-flow, through fully turbulent mass-flow and sheet flow to cohesive mass-flow deposits and then a return of braided-stream alluvium at the top of the sequence. The fan wedge demonstrates the wide range of textures possible within a ‘mass-flow” system. |
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