{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2024,11,20]],"date-time":"2024-11-20T05:34:02Z","timestamp":1732080842311,"version":"3.28.0"},"reference-count":37,"publisher":"Geological Society of London","issue":"1","license":[{"start":{"date-parts":[[1988,6,1]],"date-time":"1988-06-01T00:00:00Z","timestamp":581126400000},"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":[[1988,6]]},"abstract":"<jats:title>Synopsis<\/jats:title>\n          <jats:p>The Scaraben area contains a continuous sequence of metasediments which include psammites and semi-pelites, of undoubted Moine affinities, and the Scaraben Quartzite which several workers have assigned to the Dalradian. These metasediments have undergone a common tectono-metamorphic history, involving four phases of deformation (D1\u2013D4) and associated amphibolite-facies metamorphism. Four different phases of granite intrusion have been identified. The Scaraben Quartzite is assigned to the \u2018old Moine\u2019 of the Northern Highlands: there is no evidence that it is an outlier of the Dalradian NW of the Great Glen Fault.<\/jats:p>","DOI":"10.1144\/sjg24010001","type":"journal-article","created":{"date-parts":[[2010,1,15]],"date-time":"2010-01-15T00:30:59Z","timestamp":1263515459000},"page":"1-13","update-policy":"http:\/\/dx.doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":8,"title":["The metamorphic rocks of the Scaraben area, East Sutherland and Caithness"],"prefix":"10.1144","volume":"24","author":[{"given":"Robin A.","family":"Strachan","sequence":"first","affiliation":[{"name":"Department of Geology and Physical Sciences, Oxford Polytechnic, Oxford OX3 0BP"}]}],"member":"1881","published-online":{"date-parts":[[2022,6,7]]},"reference":[{"key":"e_1_2_1_2_1","doi-asserted-by":"publisher","DOI":"10.1144\/sjg12010035"},{"key":"e_1_2_1_3_1","doi-asserted-by":"publisher","DOI":"10.1007\/978-1-4613-2347-1_7"},{"key":"e_1_2_1_4_1","doi-asserted-by":"publisher","DOI":"10.1130\/0016-7606(1986)97<754:CDTIAP>2.0.CO;2"},{"key":"e_1_2_1_5_1","doi-asserted-by":"publisher","DOI":"10.1180\/minmag.1971.038.296.06"},{"key":"e_1_2_1_6_1","doi-asserted-by":"publisher","DOI":"10.1029\/TC003i003p00347"},{"key":"e_1_2_1_7_1","doi-asserted-by":"publisher","DOI":"10.1016\/0040-1951(77)90085-3"},{"key":"e_1_2_1_8_1","doi-asserted-by":"publisher","DOI":"10.1017\/S0080456800017853"},{"key":"e_1_2_1_9_1","doi-asserted-by":"publisher","DOI":"10.1016\/0040-1951(74)90083-3"},{"key":"e_1_2_1_10_1","first-page":"31","article-title":"Possible dextral movements on the Great Glen and Minch faults in Scotland","volume":"240","author":"GARSON M. 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Lond. 8, 117\u201328."},{"key":"e_1_2_1_17_1","unstructured":"McCOURT W. J. 1980. The geology of the Strath Halladale\u2013Altnabreac district. Inst. Geol. Sci. Environmental Protection Unit Rep. No. 80\u20131 (open file)."},{"key":"e_1_2_1_18_1","doi-asserted-by":"publisher","DOI":"10.1017\/S0016756800057459"},{"key":"e_1_2_1_19_1","first-page":"575","volume-title":"Igneous rocks of the British Isles","author":"PANKHURST R. J.","year":"1982","unstructured":"PANKHURST R. J. 1982. Geochronological tables for British igneous rocks. In , Sutherland D. S. (ed) Igneous rocks of the British Isles, John Wiley and Sons, Chichester, 575\u201381."},{"key":"e_1_2_1_20_1","doi-asserted-by":"publisher","DOI":"10.1016\/0012-821X(74)90014-4"},{"key":"e_1_2_1_21_1","first-page":"183","volume-title":"Geol. J. Spec. Issue","author":"PIDGEON R. T.","year":"1978","unstructured":"PIDGEON R. T., AFTALION M. 1978. Cogenetic and inherited zircon U-Pb systems in granites of Scotland and England. In , Bowes D. 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