{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,10,4]],"date-time":"2025-10-04T14:05:11Z","timestamp":1759586711547,"version":"3.37.3"},"reference-count":88,"publisher":"Geological Society of London","issue":"2","license":[{"start":{"date-parts":[[2014,10,1]],"date-time":"2014-10-01T00:00:00Z","timestamp":1412121600000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["SJG"],"published-print":{"date-parts":[[2014,10]]},"abstract":"<jats:title>Synopsis<\/jats:title>\n          <jats:p>\n            The Caledonian Orogen in northern Scotland comprises two major thrust nappes: the Moine and the Sgurr Beag Nappe. The Moine Nappe contains early Neoproterozoic Morar Group rocks (Moine Supergroup) and basement inliers. This paper describes the structure and stratigraphy of the Knoydart peninsula, a key area within the southern Moine Nappe. The geology of Knoydart is dominated by a thick internally coherent sequence of Morar Group rocks. This sequence is shown to be deformed by large-scale, west-vergent and west-facing Caledonian (early Palaeozoic) folds that represent D\n            <jats:sub>2<\/jats:sub>\n            within the southern Moine Nappe. Subsequent D\n            <jats:sub>3<\/jats:sub>\n            deformation led to refolding or tightening of F\n            <jats:sub>2<\/jats:sub>\n            folds, so that the major Morar Antiform is, in essence, a composite F\n            <jats:sub>2<\/jats:sub>\n            \/F\n            <jats:sub>3<\/jats:sub>\n            fold. F\n            <jats:sub>2<\/jats:sub>\n            and F\n            <jats:sub>3<\/jats:sub>\n            folds are broadly co-axial, but F\n            <jats:sub>3<\/jats:sub>\n            folds have steeper axial planes. The F\n            <jats:sub>2<\/jats:sub>\n            \/F\n            <jats:sub>3<\/jats:sub>\n            folds refold a regional-scale, originally recumbent, isoclinal F\n            <jats:sub>1<\/jats:sub>\n            fold nappe of probable Knoydartian (mid-Neoproterozoic) age. The F\n            <jats:sub>1<\/jats:sub>\n            fold nappe is cored by a thin sliver of basement gneiss; the lower limb comprises migmatitic Morar Group rocks, exposed in the Morar Window. The upper limb of the F\n            <jats:sub>1<\/jats:sub>\n            fold nappe occupies most of Knoydart and is stratigraphically coherent and right-way-up. Within this sequence, the upper unit of the Lower Morar Psammite is barely deformed, preserving trough-cross-bedding and large-scale channels in thick beds. This suggests braided river deposition, similar to the Torridon Group west of the Moine Thrust and the Morar Group in the northern part of the Moine Nappe. On the basis of lithological similarity and stratigraphic disposition, it is suggested that the lowermost part of the Morar Group in Knoydart correlates with the Neoproterozoic Sleat Group on Skye.\n          <\/jats:p>","DOI":"10.1144\/sjg2014-002","type":"journal-article","created":{"date-parts":[[2014,10,31]],"date-time":"2014-10-31T11:36:03Z","timestamp":1414755363000},"page":"125-142","source":"Crossref","is-referenced-by-count":6,"title":["Structure and stratigraphy of the Morar Group in Knoydart, NW Highlands: implications for the history of the Moine Nappe and stratigraphic links between the Moine and Torridonian successions"],"prefix":"10.1144","volume":"50","author":[{"given":"M.","family":"Krabbendam","sequence":"first","affiliation":[{"name":"British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3LA, UK"}]},{"given":"A. G.","family":"Leslie","sequence":"additional","affiliation":[{"name":"British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3LA, UK"}]},{"given":"K. M.","family":"Goodenough","sequence":"additional","affiliation":[{"name":"British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3LA, UK"}]}],"member":"1881","published-online":{"date-parts":[[2014,10,17]]},"reference":[{"key":"e_1_3_2_2_1","doi-asserted-by":"publisher","DOI":"10.1017\/S0016756800020033"},{"key":"e_1_3_2_3_1","first-page":"253","volume-title":"Continental Tectonics and Mountain Building: The Legacy of Peach and Horne","author":"Alsop G.I.","year":"2010","unstructured":"Alsop G.I., Cheer D.C., Strachan R.A., Krabbendam M., Kinny P.D., Holdsworth R.E., Leslie A.G. 2010. Progressive fold and fabric evolution associated with regional strain gradients: A case study from across a Scandian ductile thrust nappe, Scottish Caledonides. In: , Law R., Butler R.W.H., Holdsworth R.E., Krabbendam M., Strachan R.A. (eds) Continental Tectonics and Mountain Building: The Legacy of Peach and Horne. Geological Society, London, Special Publications, 335, 253\u2013272."},{"key":"e_1_3_2_4_1","doi-asserted-by":"publisher","DOI":"10.1144\/transed.16.2.93"},{"key":"e_1_3_2_5_1","series-title":"Geological Conservation Review Series","first-page":"502","volume-title":"Lewisian, Torridonian and Moine rocks of Scotland","author":"Barber A.J.","year":"2009","unstructured":"Barber A.J. 2009. Attadale. In: , Mendum J.R., A.J. , et al. . (eds) Lewisian, Torridonian and Moine rocks of Scotland. Geological Conservation Review Series, 34. 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