{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2024,11,20]],"date-time":"2024-11-20T05:34:49Z","timestamp":1732080889056,"version":"3.28.0"},"reference-count":21,"publisher":"Geological Society of London","issue":"2","license":[{"start":{"date-parts":[[1991,12,1]],"date-time":"1991-12-01T00:00:00Z","timestamp":691545600000},"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":[[1991,12]]},"abstract":"<jats:title>Synopsis<\/jats:title>\n          <jats:p>The S\u00edofra Gabbro, considered to be of Paleocene age, is exposed on the now uplifted late-Tertiary erosion surface of the West Connacht plateau. It is a vertical cylindrical body emplaced into near-vertical Ordovician slates that carry a mild thermal aurcole. The intrusion is composed of labradorite-augite-olivine-leucogabbro containing cognate mafic xenocrysts. Although \u2018Mg\u2019 values close to 60 indicate a similar degree of magmatic evolution to that of the coeval alkaline dolerite dyke systems of West Connacht, the gabbro is distinctively subalkaline. It is also relatively enriched in alumina and depleted in both compatible and incompatible trace elements. The S\u00edofra magma appears to have rested and fractionated at the top of a zoned belljar chamber in the upper crust.<\/jats:p>","DOI":"10.1144\/sjg27020127","type":"journal-article","created":{"date-parts":[[2010,1,15]],"date-time":"2010-01-15T00:30:59Z","timestamp":1263515459000},"page":"127-133","update-policy":"http:\/\/dx.doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":2,"title":["The S\u00edofra Gabbro, West Connacht, Ireland"],"prefix":"10.1144","volume":"27","author":[{"given":"Paul","family":"Mohr","sequence":"first","affiliation":[{"name":"Department of Geology, University College Galway, Galway, Ireland"}]}],"member":"1881","published-online":{"date-parts":[[2022,6,7]]},"reference":[{"key":"e_1_2_1_2_1","doi-asserted-by":"publisher","DOI":"10.1093\/petrology\/21.4.629"},{"key":"e_1_2_1_3_1","doi-asserted-by":"publisher","DOI":"10.1144\/gsjgs.119.1.0313"},{"key":"e_1_2_1_4_1","unstructured":"GRAHAM J. LEAKE B. E. RYAN P. D. 1985. Geological map of South Mayo (1:63 360). Univ. Glasgow."},{"key":"e_1_2_1_5_1","doi-asserted-by":"publisher","DOI":"10.1017\/S0016756800053024"},{"key":"e_1_2_1_6_1","doi-asserted-by":"publisher","DOI":"10.1093\/petrology\/24.4.605"},{"key":"e_1_2_1_7_1","doi-asserted-by":"crossref","unstructured":"KINAHAN G. H. SYMES R. G. WARREN J. L. WILKINSON S. B. NOLAN J. LEONARD H. 1874. Geological map sheet 84 (1:63 360). Geol. Surv. Ireland.","DOI":"10.1017\/S0016756800169663"},{"key":"e_1_2_1_8_1","unstructured":"KINAHAN G. H. SYMES R. G. WILKINSON S. B. NOLAN J. LEONARD H. 1876. Explanatory memoir to accompany sheets 73 and 74 (in part) 83 and 84 including the country around Westport Eriff Valley Killary Harbour and western shores of Lough Mask. Mem. Geol. Surv. 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