{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2024,11,20]],"date-time":"2024-11-20T05:33:19Z","timestamp":1732080799917,"version":"3.28.0"},"reference-count":35,"publisher":"Geological Society of London","issue":"1","license":[{"start":{"date-parts":[[1968,2,1]],"date-time":"1968-02-01T00:00:00Z","timestamp":-60480000000},"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":[[1968,2]]},"abstract":"<jats:title>Synopsis<\/jats:title>\n          <jats:p>\n            A nepheline normative eclogite containing almandine-rich garnet and Na\n            <jats:sub>2<\/jats:sub>\n            O-rich (5.47 per cent) pyroxene is described. The origin of the Glenelg eclogites is reviewed and an hypothesis of tectonic emplacement from a deeper metamorphic source in the uppermost mantle preferred. It is suggested that the rocks were originally basic magmas or accumulates from such magmas originally crystallised near the crust-mantle boundary.\n          <\/jats:p>","DOI":"10.1144\/sjg04010001","type":"journal-article","created":{"date-parts":[[2010,1,15]],"date-time":"2010-01-15T00:29:39Z","timestamp":1263515379000},"page":"1-9","update-policy":"http:\/\/dx.doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":7,"title":["Nepheline normative eclogite from Loch Duich, Ross-shire"],"prefix":"10.1144","volume":"4","author":[{"given":"E. L. P.","family":"Mercy","sequence":"first","affiliation":[{"name":"Grant Institute of Geology, University of Edinburgh"}]},{"given":"M. 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