{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2024,11,20]],"date-time":"2024-11-20T05:33:59Z","timestamp":1732080839686,"version":"3.28.0"},"reference-count":15,"publisher":"Geological Society of London","issue":"2","license":[{"start":{"date-parts":[[1971,8,1]],"date-time":"1971-08-01T00:00:00Z","timestamp":49852800000},"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":[[1971,8]]},"abstract":"<jats:title>Synopsis<\/jats:title>\n          <jats:p>A Tertiary tholeiitic dyke intruded into sedimentary rocks of Lower Carboniferous age is locally rich in xenoliths of siliceous and argillaceous rocks possibly of Upper Old Red Sandstone age. The xenoliths and the country rocks have suffered thermal metamorphism with the production of glass, tridymite, cordierite, pyroxenes and biotite in the former and tridymite, cordierite, biotite and lime-garnet in the latter. From considerations of the stability fields of tridymite, melt-products and the solidus of dolerite, it is estimated that the PT conditions under which the presently exposed levels of the dyke crystallised were approximately 500 bars and 1,000\u00b0 C, possibly representing a cover in Tertiary times some 6,200 ft (1,900 m) thick.<\/jats:p>","DOI":"10.1144\/sjg07020153","type":"journal-article","created":{"date-parts":[[2010,1,15]],"date-time":"2010-01-15T00:29:39Z","timestamp":1263515379000},"page":"153-161","update-policy":"http:\/\/dx.doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":0,"title":["A xenolithic dyke at M\u2019Inroy\u2019s Point, Gourock, Renfrewshire"],"prefix":"10.1144","volume":"7","author":[{"given":"A.","family":"Herriot","sequence":"first","affiliation":[{"name":"3 Glen Bervie, St. Leonards, East Kilbride"}]}],"member":"1881","published-online":{"date-parts":[[2022,6,7]]},"reference":[{"key":"e_1_2_1_2_1","doi-asserted-by":"publisher","DOI":"10.1144\/GSL.JGS.1944.100.01-04.13"},{"key":"e_1_2_1_3_1","first-page":"533","article-title":"Melting relations of Tertiary granitic rocks in Skye and Rhum","volume":"33","author":"BROWN G. 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London.","edition":"3"},{"key":"e_1_2_1_9_1","first-page":"1788","article-title":"System CaO-Al2O3-SiO2-H2O. VI: The grossularite-3CaO.Al2-O36H2O join","volume":"68","author":"ROY D. M.","year":"1957","unstructured":"ROY D. M., ROY R. 1957. System CaO-Al2O3-SiO2-H2O. VI: The grossularite-3CaO.Al2-O36H2O join. Bull. geol. Soc. Amer. 68, 1788\u20139 (abstract).","journal-title":"Bull. geol. Soc. Amer"},{"key":"e_1_2_1_10_1","first-page":"271","article-title":"The system Mg-cordierite-H2O and related rocks","volume":"101","author":"SCHREYER W.","year":"1964","unstructured":"SCHREYER W., YODER H. S. 1964. The system Mg-cordierite-H2O and related rocks. N. Jb. Miner. Abh. 101, 271\u2013342.","journal-title":"N. Jb. Miner. Abh"},{"key":"e_1_2_1_11_1","first-page":"263","article-title":"A granophyre from Coire Uaigneich, Isle of Skye, containing quartz paramorphs after tridymite","volume":"30","author":"WAGER L. R.","year":"1953","unstructured":"WAGER L. R., WEEDON D. S., VINCENT A. E. 1953. A granophyre from Coire Uaigneich, Isle of Skye, containing quartz paramorphs after tridymite. Mineralog. Mag. 30, 263\u201376.","journal-title":"Mineralog. Mag"},{"key":"e_1_2_1_12_1","doi-asserted-by":"publisher","DOI":"10.1007\/978-3-662-00866-9"},{"key":"e_1_2_1_13_1","first-page":"1039","article-title":"Microscopic cordierite in fused Torridonian arkose","volume":"44","author":"WYLLIE P. J.","year":"1959","unstructured":"WYLLIE P. J. 1959. Microscopic cordierite in fused Torridonian arkose. Amer. Min. 44, 1039\u201346.","journal-title":"Amer. Min"},{"key":"e_1_2_1_14_1","doi-asserted-by":"publisher","DOI":"10.1093\/petrology\/2.1.1"},{"key":"e_1_2_1_15_1","doi-asserted-by":"publisher","DOI":"10.1017\/S0016756800000078"},{"key":"e_1_2_1_16_1","doi-asserted-by":"publisher","DOI":"10.1093\/petrology\/3.3.342"}],"container-title":["Scottish Journal of Geology"],"original-title":[],"language":"en","link":[{"URL":"https:\/\/www.lyellcollection.org\/doi\/pdf\/10.1144\/sjg07020153","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2024,11,19]],"date-time":"2024-11-19T16:48:27Z","timestamp":1732034907000},"score":1,"resource":{"primary":{"URL":"https:\/\/www.lyellcollection.org\/doi\/10.1144\/sjg07020153"},"secondary":[{"URL":"https:\/\/geoscienceworld.org\/sjg\/article-lookup?doi=10.1144\/sjg07020153","label":"geoscienceworld"}]},"subtitle":[],"short-title":[],"issued":{"date-parts":[[1971,8]]},"references-count":15,"journal-issue":{"issue":"2","published-online":{"date-parts":[[2009,11,10]]},"published-print":{"date-parts":[[1971,8]]}},"alternative-id":["10.1144\/sjg07020153"],"URL":"https:\/\/doi.org\/10.1144\/sjg07020153","relation":{},"ISSN":["0036-9276","2041-4951"],"issn-type":[{"type":"print","value":"0036-9276"},{"type":"electronic","value":"2041-4951"}],"subject":[],"published":{"date-parts":[[1971,8]]},"assertion":[{"value":"1969-01-30","order":0,"name":"received","label":"Received","group":{"name":"publication_history","label":"Publication History"}},{"value":"1970-10-15","order":1,"name":"revised","label":"Revised","group":{"name":"publication_history","label":"Publication History"}},{"value":"2022-06-07","order":3,"name":"published","label":"Published","group":{"name":"publication_history","label":"Publication History"}}]}}