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The integration of U\u2013Pb and Hf isotope analyses in detrital zircon crystals reduces potential ambiguities arising from non-unique age populations and yields information on the crustal evolution of the source terranes. Samples of basal ORS successions yield zircon U\u2013Pb age groupings of\n            <jats:italic>c.<\/jats:italic>\n            1800\u20131500 and\n            <jats:italic>c.<\/jats:italic>\n            1200\u2013900\u2005Ma, with minor Neoarchean, Tonian, Ediacaran and Ordovician contributions. SW Baltica provides the best match for detrital zircon ages and Hf isotopic signatures and much of the &gt;900\u2005Ma zircon population was probably recycled from Neoproterozoic successions.\n            <jats:italic>\u03b5<\/jats:italic>\n            Hf\n            <jats:sub>\n              (\n              <jats:italic>t<\/jats:italic>\n              )\n            <\/jats:sub>\n            values in\n            <jats:italic>c.<\/jats:italic>\n            1800\u20131000\u2005Ma grains reflect the assembly of Nuna, the development of a long-lived retreating subduction system along its margin and Grenville collisional orogenesis. These basal ORS successions were probably deposited within the same regional fluvial system as coeval sedimentary rocks in the Midland Valley, draining an area of positive relief in SW Baltica where continental convergence continued through the Early Devonian.\n          <\/jats:p>\n          <jats:p content-type=\"supplementary-material\">\n            <jats:bold>Supplementary material<\/jats:bold>\n            : Isotopic data, statistical comparison of selected samples and TIMA heavy mineral data are available at\n            <jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" ext-link-type=\"uri\" specific-use=\"dataset is-supplemented-by\" xlink:href=\"https:\/\/doi.org\/10.6084\/m9.figshare.c.5301780\">https:\/\/doi.org\/10.6084\/m9.figshare.c.5301780<\/jats:ext-link>\n          <\/jats:p>","DOI":"10.1144\/jgs2020-241","type":"journal-article","created":{"date-parts":[[2021,2,16]],"date-time":"2021-02-16T12:00:57Z","timestamp":1613476857000},"update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":11,"title":["Evidence from the U\u2013Pb\u2013Hf signatures of detrital zircons for a Baltican provenance for basal Old Red Sandstone successions, northern Scottish Caledonides"],"prefix":"10.1144","volume":"178","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-9568-0832","authenticated-orcid":false,"given":"Rob A.","family":"Strachan","sequence":"first","affiliation":[{"name":"School of the Environment, Geography and Geosciences, University of Portsmouth, Burnaby Road, Portsmouth PO1 3QL, UK"},{"name":"Timescales of Mineral Systems Group, Centre for Exploration Targeting \u2013 Curtin Node, School of Earth and Planetary Sciences, Curtin University, GPO Box U1987, Perth, WA 6845, Australia"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-5961-4304","authenticated-orcid":false,"given":"Hugo K. 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