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• W2076708608 abstract "Abstract The succession, lithological variation and original structures of the Torridonian of part of the Kishom Nappe in Skye are discussed with special reference to features which may throw light on regional variations in the formation. It is found that most of the stratigraphical sub-divisions established by Clough show distinctive associations of sedimentary structures, which are described. The thickness of the succession appears to be rather greater than has previously been supposed and a figure of about 10,000 feet is suggested for the Diabaig Group or Lower Torridonian. The directions of current flow indicated by current- and ripple-drift bedding and the orientation of ripple-marks are recorded. In the Diabaig Group, flow along lines between north-east/south-west and north/south predominates, but current-bedding in the Beinn na Seamraig sub-division indicates flow from the north-north-west. In the Applecross Group the dominant flow is from the north-west. In Moine and Tarskavaig Moine rocks of Morar, Glenelg and Skye, many types of sedimentation structures, including distinctive disturbances related to movement of quicksands, closely resemble those occurring in the Torridonian. The Moine and Torridonian successions are compared and it is concluded that while the broad distinction between Diabaig and Applecross Groups may be reflected in the Moine sequence no precise matching of sub-divisions is possible. Evidence of lateral variation within the Kishorn Nappe and from this nappe to the Tarskavaig and Moine nappes is discussed." @default.
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• W2076708608 date "1964-01-01" @default.
• W2076708608 modified "2023-09-28" @default.
• W2076708608 title "Some aspects of Torridonian stratigraphy in Skye" @default.
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• W2076708608 doi "https://doi.org/10.1016/s0016-7878(64)80033-x" @default.
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