{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2024,9,16]],"date-time":"2024-09-16T18:43:43Z","timestamp":1726512223421},"reference-count":42,"publisher":"Geological Society of London","issue":"1","license":[{"start":{"date-parts":[[2014,4,9]],"date-time":"2014-04-09T00:00:00Z","timestamp":1397001600000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["SJG"],"published-print":{"date-parts":[[2014,5]]},"abstract":"<jats:title>Synopsis<\/jats:title>\n          <jats:p>The Bracken Bay\u2013Straiton dyke, a member of the Palaeogene Mull dyke swarm, is one of the Solitary dykes of southern Scotland and northern England recognized by Geikie (1897). It shows a remarkable (unique?) change of strike direction, deviating from the regional NW\u2013SE trend to propagate along the Southern Upland Fault for 16\u2009km before apparently resuming its southeasterly course in the Southern Uplands. The dyke is a clinopyroxene\u2013plagioclase\u2013phyric quartz tholeiite, showing little petrographic variation along strike. However, geochemical data indicate that the dyke segment south of the Southern Upland Fault is not comagmatic with the main dyke; it is here distinguished as the Kello Water dyke. The reason for the dyke\u2019s deviation at the fault is uncertain but may be related to a significant role for crustal heterogeneities, particularly Caledonian fractures which had earlier been utilized by the Late Carboniferous quartz dolerite dyke swarm.<\/jats:p>\n          <jats:sec>\n            <jats:title>Supplementary material:<\/jats:title>\n            <jats:p>\n              Electron microprobe analysis data are available at\n              <jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" ext-link-type=\"uri\" xlink:href=\"http:\/\/www.geolsoc.org.uk\/SUP18737\">http:\/\/www.geolsoc.org.uk\/SUP18737<\/jats:ext-link>\n              .\n            <\/jats:p>\n          <\/jats:sec>","DOI":"10.1144\/sjg2013-009","type":"journal-article","created":{"date-parts":[[2014,5,23]],"date-time":"2014-05-23T11:36:03Z","timestamp":1400844963000},"page":"57-69","source":"Crossref","is-referenced-by-count":4,"title":["The Palaeogene Bracken Bay\u2013Straiton dyke: composition and controls on intrusion"],"prefix":"10.1144","volume":"50","author":[{"given":"R.","family":"MacDonald","sequence":"first","affiliation":[{"name":"Institute of Mineralogy, Geochemistry and Petrology, University of Warsaw, 02-089 Warszawa, Poland"},{"name":"Environment Centre, Lancaster University, Lancaster LA14YQ, UK"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"B.","family":"Bagi\u0144ski","sequence":"additional","affiliation":[{"name":"Institute of Mineralogy, Geochemistry and Petrology, University of Warsaw, 02-089 Warszawa, Poland"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"D. A.","family":"MacInnes","sequence":"additional","affiliation":[{"name":"3 Stirling Road, Kilsyth, Glasgow G65 0JF, UK"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"J. C.","family":"MacGillivray","sequence":"additional","affiliation":[{"name":"Hollandbush, 4 Meadowbank Avenue, Strathaven, Lanarkshire ML10 6JS, Scotland, UK"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"D. J.","family":"Fettes","sequence":"additional","affiliation":[{"name":"British Geological Survey, Murchison House, West Mains Road, Edinburgh EH9 3EH, Scotland, UK"}],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"1881","published-online":{"date-parts":[[2014,4,9]]},"reference":[{"key":"e_1_3_3_2_1","volume-title":"The Dynamics of Faulting","author":"Anderson E. M.","year":"1951","unstructured":"Anderson E. M. 1951. The Dynamics of Faulting (2nd edn). 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