{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,11,3]],"date-time":"2025-11-03T09:09:29Z","timestamp":1762160969325},"reference-count":84,"publisher":"Geological Society of London","issue":"6","license":[{"start":{"date-parts":[[2012,11,1]],"date-time":"2012-11-01T00:00:00Z","timestamp":1351728000000},"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":["JGS"],"published-print":{"date-parts":[[2012,11]]},"abstract":"<jats:p>\n            Detrital U\u2013Pb laser ablation inductively coupled plasma mass spectrometry zircon ages from six siliciclastic samples from the lower allochthon of NW Iberia are analysed to constrain their maximum sedimentation age and provenance, and to evaluate the connections to the adjacent tectonostratigraphic domains. Deposited in the external sections of the Gondwana platform, their maximum depositional age is latest Neoproterozoic (\n            <jats:italic>c<\/jats:italic>\n            . 560\u2009Ma). Comparison of the age populations of the lower allochthon with those of the rest of the allochthonous and autochthonous units of NW Iberia suggests that the terranes located in the footwall of the Variscan suture should not be considered as exotic elements, but as contiguous pieces of the same continental margin transported onto the adjacent Gondwana mainland in Variscan times. The data are in agreement with the regional trend defined by the drop in Early Neoproterozoic and Mesoproterozoic zircon content upward in the tectonic pile, which had been previously proposed as a marker of proximity to the eastern part of the West African Craton. Based on the age spectra, the palaeoposition for the time of sedimentation is placed in northern Africa, between the West African and Saharan cratons. Particular attention is paid to the occurrence of an Early Neoproterozoic input, probably derived from the Pan-African Hoggar suture.\n          <\/jats:p>\n          <jats:sec>\n            <jats:title>Supplementary materials:<\/jats:title>\n            <jats:p>\n              Isotope ratios and ages for the selected analyses 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\/SUP18548\">www.geolsoc.org.uk\/SUP18548<\/jats:ext-link>\n              .\n            <\/jats:p>\n          <\/jats:sec>","DOI":"10.1144\/jgs2011-146","type":"journal-article","created":{"date-parts":[[2012,11,1]],"date-time":"2012-11-01T14:29:49Z","timestamp":1351780189000},"page":"655-665","source":"Crossref","is-referenced-by-count":55,"title":["U\u2013Pb detrital zircon analysis of the lower allochthon of NW Iberia: age constraints, provenance and links with the Variscan mobile belt and Gondwanan cratons"],"prefix":"10.1144","volume":"169","author":[{"given":"Rub\u00e9n","family":"D\u00edez Fern\u00e1ndez","sequence":"first","affiliation":[{"name":"Departamento de Geolog\u00eda, Universidad de Salamanca, 37008 Salamanca, Spain"}]},{"given":"Jos\u00e9 R.","family":"Mart\u00ednez Catal\u00e1n","sequence":"additional","affiliation":[{"name":"Departamento de Geolog\u00eda, Universidad de Salamanca, 37008 Salamanca, Spain"}]},{"given":"Ricardo","family":"Arenas","sequence":"additional","affiliation":[{"name":"Departamento de Petrolog\u00eda y Geoqu\u00edmica and Instituto de Geolog\u00eda Econ\u00f3mica, Universidad Complutense\/Consejo Superior de Investigaciones Cient\u00edficas, 28040 Madrid, Spain"}]},{"given":"Jacobo","family":"Abati","sequence":"additional","affiliation":[{"name":"Departamento de Petrolog\u00eda y Geoqu\u00edmica and Instituto de Geolog\u00eda Econ\u00f3mica, Universidad Complutense\/Consejo Superior de Investigaciones Cient\u00edficas, 28040 Madrid, Spain"}]},{"given":"Axel","family":"Gerdes","sequence":"additional","affiliation":[{"name":"Institut f\u00fcr Geowissenschaften, Mineralogie, Goethe-Universit\u00e4t, D-60438 Frankfurt am Main, Germany"},{"name":"Department of Earth Sciences, Stellenbosch University, Private Bag X1, Matieland 7602, South Africa"}]},{"given":"Javier","family":"Fern\u00e1ndez-Su\u00e1rez","sequence":"additional","affiliation":[{"name":"Departamento de Petrolog\u00eda y Geoqu\u00edmica and Instituto de Geolog\u00eda Econ\u00f3mica, Universidad Complutense\/Consejo Superior de Investigaciones Cient\u00edficas, 28040 Madrid, Spain"}]}],"member":"1881","published-online":{"date-parts":[[2012,11]]},"reference":[{"key":"e_1_3_2_2_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0012-821X(98)00268-4"},{"key":"e_1_3_2_3_1","doi-asserted-by":"publisher","DOI":"10.1130\/B26572.1"},{"key":"e_1_3_2_4_1","first-page":"23","article-title":"Caracterizaci\u00f3n de las rocas metavolc\u00e1nicas sil\u00faricas del NO del Macizo Ib\u00e9rico","volume":"3","author":"Ancochea E.","year":"1988","unstructured":"Ancochea E., Arenas R., Brandle J.L., Peinado M., Sagredo J. 1988. 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