{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,3,24]],"date-time":"2026-03-24T20:32:46Z","timestamp":1774384366553,"version":"3.50.1"},"reference-count":56,"publisher":"Geological Society of London","issue":"2","license":[{"start":{"date-parts":[[1986,10,1]],"date-time":"1986-10-01T00:00:00Z","timestamp":528508800000},"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":[[1986,10]]},"abstract":"<jats:title>Synopsis<\/jats:title>\n          <jats:p>\n            The c. 6 km\n            <jats:sup>2<\/jats:sup>\n            complex comprises graphitic\/pyritic, mainly kyanite-rich pelites, interbanded with metalimestones and invaded by foliated serpentinites. It is enveloped by typically Moinian psammites, semipelites and pelites. Previously regarded as a Lewisian inlier, or as integral to the Moine succession, or as a transitional Moinian\u2013Dalradian or Dalradian\u2013Durness Limestone facies, its allochthonous status is in fact suggested by (1) its singular lithology; (2) its unique association with a large serpentinite; (3) associated sharp and local gravity and magnetic anomalies; (4) a blastomylonitic slide zone separating the complex from its Moine envelope; (5) local and regional petrological differences between pelites of the complex and Moine succession. A previous model, in which muscovite-rich Moine pelites developed by K-metasomatism (\u2018granitisation\u2019) of kyanite-schists within the complex, via (a) shimmerisation (conversion of kyanite to shimmer aggregate); and (b) coarsening of shimmer aggregate to muscovite, is ruled out by new whole-rock and microprobe data. These suggest shimmerisation was a near-isochemical, small-scale redistribution of alkalis and water [approximately\n            <jats:italic>kyanite<\/jats:italic>\n            +\n            <jats:italic>biotite<\/jats:italic>\n            +\n            <jats:italic>quartz<\/jats:italic>\n            +\n            <jats:italic>water<\/jats:italic>\n            =\n            <jats:italic>muscovite<\/jats:italic>\n            (\n            <jats:italic>shimmer aggregate<\/jats:italic>\n            ) +\n            <jats:italic>chlorite<\/jats:italic>\n            ], and show large compositional differences between shimmer aggregates and coarse muscovites. Rb\u2013Sr isotopic data imply Late Caledonian (c. 459 Ma) metamorphism in the complex, but also imply a significant earlier history for the kyanite-schists. Overall, data not merely invalidate a Glen Urquhart \u2018Lewisian inlier\u2019, but also as yet preclude correlation of the complex with the Moine or Dalradian. It is attributed in the interim to a separate lithotectonic unit, the \u2018Albynian\u2019, which may lie between (or be diachronous with) some part of the Moinian or Dalradian successions.\n          <\/jats:p>","DOI":"10.1144\/sjg22020179","type":"journal-article","created":{"date-parts":[[2010,1,15]],"date-time":"2010-01-15T00:30:59Z","timestamp":1263515459000},"page":"179-202","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":6,"title":["Pelites of the Glen Urquhart serpentinite\u2013metamorphic complex, west of Loch Ness (Anomalous local limestone\u2013pelite successions within the Moine outcrop: III)"],"prefix":"10.1144","volume":"22","author":[{"given":"N. M. 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