Reconstruction of the ordovician pakhuis ice sheet, South Africa

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dc.contributor.authorBlignault H.J.
dc.contributor.authorTheron J.N.
dc.date.accessioned2011-05-15T16:00:33Z
dc.date.available2011-05-15T16:00:33Z
dc.date.issued2010
dc.description.abstractThis reconstruction of the Late Ordovician, glacigenic Pakhuis Formation of the Table Mountain Group is based on a variety of diverse datasets. Field observations were made over the full 300 km extent of exposure in a north-south direction. The thin glacigenic package constitutes a minor interlude in the development of a subcontinental, Palaeozoic, siliciclastic basin. The Pakhuis Formation is of special interest because it includes features like the extensive penecontemporaneous folding, an erosional unconformity and the uniform lithological character of the sandy diamictites. A model is presented by which an unusual concurrence of circumstances produced the special features of the Pakhuis glacigenics. These are the ice invasion of a developing basin, an onset zone within basin and a deep trough harboring an ice-stream. Subglacial, grounding zone and iceberg facies associations with their lateral variations are developed. The temperate, glaciation of relative short duration, comprised one major and a second minor advance. During the first advance the grounded ice sheet with slow-moving sheet-flow reached ice-stream characteristics along at least part of a trough. The occurrence of an ice-stream within a slow-moving, low-profile ice sheet provides the glaciological environment for ice-stream draw-down, flanking infill of ice, resulting in compressional ice-flow from the sides. The fundamental requirement for buckling (i.e. the development of the Fold Zone) is layer parallel shortening achieved by the compressional ice-flow. Ice-bed interface features like deforming-bed structures are developed, as well as outsize flutes for which an alternative bulk strain model is proposed. The glacial retreat was rapid, interrupted only by the second, minor advance. A marine environment is attested by the postglacial fauna of a black shale. © 2010 September Geological Society of South Africa.
dc.description.versionArticle
dc.identifier.citationSouth African Journal of Geology
dc.identifier.citation113
dc.identifier.citation3
dc.identifier.issn10120750
dc.identifier.other10.2113/gssajg.113.3.335
dc.identifier.urihttp://hdl.handle.net/10019.1/11760
dc.subjectbasin evolution
dc.subjectglacier advance
dc.subjectglacier retreat
dc.subjectice sheet
dc.subjectice stream
dc.subjectOrdovician
dc.subjectreconstruction
dc.subjectsequence stratigraphy
dc.subjectunconformity
dc.subjectSouth Africa
dc.titleReconstruction of the ordovician pakhuis ice sheet, South Africa
dc.typeArticle
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