{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,10,1]],"date-time":"2025-10-01T16:18:56Z","timestamp":1759335536647,"version":"3.28.0"},"reference-count":29,"publisher":"Geological Society of London","issue":"1","license":[{"start":{"date-parts":[[1973,5,1]],"date-time":"1973-05-01T00:00:00Z","timestamp":105062400000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"content-domain":{"domain":["www.lyellcollection.org"],"crossmark-restriction":true},"short-container-title":["SJG"],"published-print":{"date-parts":[[1973,5]]},"abstract":"<jats:title>Synopsis<\/jats:title>\n          <jats:p>\n            The Carn Chuinneag intrusion is a foliated granite pluton emplaced in the Moine rocks of the Northern Highlands of Scotland, containing large irregular inclusions of amphibolite. Minor sheet-like apophyses at the margin of the pluton extend into the Moine country rocks. The emplacement occurred after\n            <jats:italic>D<\/jats:italic>\n            <jats:sub>1<\/jats:sub>\n            in static conditions and the Moinian envelope was distended. Structure contours suggest that the intrusion was originally a sheet-like pluton about 4 km (2.48 miles) thick.\n            <jats:italic>D<\/jats:italic>\n            <jats:sub>1<\/jats:sub>\n            structures which are ubiquitous in the Moinian over a wide area surrounding the granite are entirely absent from the pluton. The widespread foliation of the pluton and sheet-like apophyses is equivalent to\n            <jats:italic>S<\/jats:italic>\n            <jats:sub>2<\/jats:sub>\n            in the Moine rocks, and it is folded by major and minor scale\n            <jats:italic>D<\/jats:italic>\n            <jats:sub>3<\/jats:sub>\n            folds closely similar in style to\n            <jats:italic>D<\/jats:italic>\n            <jats:sub>3<\/jats:sub>\n            folds developed in the Moinian both inside and outside the granite aureole.\n            <jats:italic>D<\/jats:italic>\n            <jats:sub>4<\/jats:sub>\n            deformed the whole of the pluton and its Moinian envelope.\n            <jats:italic>D<\/jats:italic>\n            <jats:sub>1<\/jats:sub>\n            and\n            <jats:italic>D<\/jats:italic>\n            <jats:sub>2<\/jats:sub>\n            structures of the Carn Chuinneag area and the Moine Thrust belt at Loch Eriboll are considered to be correlatives. Thus, pre-granite\n            <jats:italic>D<\/jats:italic>\n            <jats:sub>1<\/jats:sub>\n            structures are inferred to be post-Arenig in age.\n          <\/jats:p>","DOI":"10.1144\/sjg09010063","type":"journal-article","created":{"date-parts":[[2010,1,15]],"date-time":"2010-01-15T00:29:39Z","timestamp":1263515379000},"page":"63-88","update-policy":"http:\/\/dx.doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":29,"title":["The structure and structural dating of the Carn Chuinneag intrusion, Ross-shire"],"prefix":"10.1144","volume":"9","author":[{"given":"J.","family":"Shepherd","sequence":"first","affiliation":[{"name":"Robertson Research (Australia) Pty. Limited, Laboratory, Moss Vale Road, Bowral, N.S.W. 2576, Australia"}]}],"member":"1881","published-online":{"date-parts":[[2022,6,7]]},"reference":[{"key":"e_1_2_1_2_1","doi-asserted-by":"publisher","DOI":"10.1130\/GSAB-45-621"},{"key":"e_1_2_1_3_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0016-7878(70)80006-2"},{"key":"e_1_2_1_4_1","first-page":"345","article-title":"The structure of the Moine Thrust zone in the Assynt region of north-west Scotland","volume":"40","author":"CHRISTIE J. M.","year":"1963","unstructured":"CHRISTIE J. M. 1963. The structure of the Moine Thrust zone in the Assynt region of north-west Scotland. Univ. Calif. Publs, geol. Sci. 40, 345\u2013440.","journal-title":"Univ. Calif. Publs, geol. 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London.","edition":"2"},{"key":"e_1_2_1_10_1","doi-asserted-by":"publisher","DOI":"10.1017\/S0016756800066279"},{"key":"e_1_2_1_11_1","doi-asserted-by":"publisher","DOI":"10.1093\/petrology\/3.2.215"},{"key":"e_1_2_1_12_1","doi-asserted-by":"publisher","DOI":"10.1144\/sjg06020226"},{"key":"e_1_2_1_13_1","unstructured":"HAUGH I. 1964. The structural and metamorphic history of the south\u2013eastern part of the Carn Chuinneag Complex Ross-shire. Univ. London Ph.D. thesis (unpubl.)."},{"key":"e_1_2_1_14_1","doi-asserted-by":"publisher","DOI":"10.1007\/BF00376047"},{"key":"e_1_2_1_15_1","doi-asserted-by":"publisher","DOI":"10.1016\/0040-1951(68)90035-8"},{"key":"e_1_2_1_16_1","doi-asserted-by":"publisher","DOI":"10.1144\/sjg06020228"},{"key":"e_1_2_1_17_1","first-page":"159","article-title":"Moinian assemblage of Scotland","volume":"12","author":"JOHNSTONE G. S.","year":"1970","unstructured":"JOHNSTONE G. S., SMITH D. I., HARRIS A. L. 1970. Moinian assemblage of Scotland. Bull. Am. Ass. Petrol. Geol. Memoir 12, 159\u2013180.","journal-title":"Bull. Am. Ass. Petrol. Geol. Memoir"},{"key":"e_1_2_1_18_1","volume-title":"The British Caledonides","author":"LONG L. E.","year":"1963","unstructured":"LONG L. E., LAMBERT R. St. J. 1963. Rb\u2013Sr isotropic ages from the Moine Series in , Johnson M. R. W., Stewart F. H. (eds.), The British Caledonides. Edinburgh and London."},{"key":"e_1_2_1_19_1","first-page":"756","article-title":"Notes on the Report of the Boulder Committee of the Royal Society of Edinburgh","volume":"11","author":"MORRISON W.","year":"1881","unstructured":"MORRISON W. 1881. Notes on the Report of the Boulder Committee of the Royal Society of Edinburgh. Proc. R. Soc. Edinb. 11, 756.","journal-title":"Proc. R. Soc. Edinb"},{"key":"e_1_2_1_20_1","article-title":"The Geology of Ben Wyvis, Carn Chuinneag, Inchbae and surrounding country","author":"PEACH B.","year":"1912","unstructured":"PEACH B., GUNN W., CLOUGH C. T., HINXMAN L. W., CRAMPTON C. 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