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We present new geochronological (laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) zircon U\u2013Pb) analyses of 36 intrusive and volcanic Cretaceous rocks, along with LA-ICP-MS apatite U\u2013Pb analyses (a medium-temperature thermochronometer) of 28 Triassic\u2013Cretaceous igneous rocks of the Antarctic Peninsula. These are complemented by new zircon Hf isotope data along with whole-rock geochemistry and isotope (Nd, Sr and Pb) data. Our results indicate that the Cretaceous igneous rocks of the Antarctic Peninsula have geochemical signatures consistent with a continental arc setting and were formed during the interval\n            <jats:italic>c.<\/jats:italic>\n            140\u201379\u2005Ma, whereas the main peak of magmatism occurred during\n            <jats:italic>c.<\/jats:italic>\n            118\u2013110\u2005Ma. Trends in\n            <jats:inline-formula>\n              <mml:math xmlns:mml=\"http:\/\/www.w3.org\/1998\/Math\/MathML\" overflow=\"scroll\">\n                <mml:mi>\u03b5<\/mml:mi>\n              <\/mml:math>\n            <\/jats:inline-formula>\n            Hf\n            <jats:sub>t<\/jats:sub>\n            (zircon) combined with elevated heat flow that remagnetized rocks and reset apatite U\u2013Pb ages suggest that Cretaceous magmatism formed within a prevailing extensional setting that was punctuated by periods of compression. A noteworthy compressive period probably occurred during\n            <jats:italic>c.<\/jats:italic>\n            147\u2013128\u2005Ma, triggered by the westward migration of South America during opening of the South Atlantic Ocean. Cretaceous arc rocks that crystallized during\n            <jats:italic>c.<\/jats:italic>\n            140\u2013100\u2005Ma define a belt that extends from southeastern Palmer Land to the west coast of Graham Land. This geographical distribution could be explained by (1) a flat slab with east-dipping subduction of the Phoenix Plate, or (2) west-dipping subduction of the lithosphere of the Weddell Sea, or (3) an allochthonous origin for the rocks of Alexander Island. A better understanding of the geological history of the pre-Cretaceous rocks of Alexander Island and the inaccessible area of the southern Weddell Sea is required.\n          <\/jats:p>\n          <jats:p content-type=\"supplementary-material\">\n            <jats:bold>Supplementary material:<\/jats:bold>\n            A description of the methods used in this study and the complete dataset 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.6089274\">https:\/\/doi.org\/10.6084\/m9.figshare.c.6089274<\/jats:ext-link>\n          <\/jats:p>","DOI":"10.1144\/jgs2022-067","type":"journal-article","created":{"date-parts":[[2022,7,18]],"date-time":"2022-07-18T11:45:14Z","timestamp":1658144714000},"update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":11,"title":["Cretaceous magmatism in the Antarctic Peninsula and its tectonic implications"],"prefix":"10.1144","volume":"180","author":[{"ORCID":"https:\/\/orcid.org\/0000-0001-6678-3173","authenticated-orcid":true,"given":"Joaquin","family":"Bastias","sequence":"first","affiliation":[{"name":"Department of Earth Sciences, University of Geneva, 1205 Gen\u00e8ve, Switzerland"},{"name":"Department of Geology, Trinity College Dublin, College Green, Dublin 2, Ireland"},{"name":"Carrera Geolog\u00eda, Facultad de Ingenier\u00eda, Universidad Andres Bello, Santiago, Chile"}]},{"given":"Richard","family":"Spikings","sequence":"additional","affiliation":[{"name":"Department of Earth Sciences, University of Geneva, 1205 Gen\u00e8ve, Switzerland"}]},{"given":"Teal","family":"Riley","sequence":"additional","affiliation":[{"name":"British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK"}]},{"given":"David","family":"Chew","sequence":"additional","affiliation":[{"name":"Department of Geology, Trinity College Dublin, College Green, Dublin 2, Ireland"}]},{"given":"Anne","family":"Grunow","sequence":"additional","affiliation":[{"name":"Byrd Polar Research Center, Ohio State University, 108 Scott Hall, 1090 Carmack Road, Columbus, OH 43210, USA"}]},{"given":"Alexey","family":"Ulianov","sequence":"additional","affiliation":[{"name":"Institute of Earth Sciences, University of Lausanne, 1015 Lausanne, Switzerland"}]},{"given":"Massimo","family":"Chiaradia","sequence":"additional","affiliation":[{"name":"Department of Earth Sciences, University of Geneva, 1205 Gen\u00e8ve, Switzerland"}]},{"given":"Alex","family":"Burton-Johnson","sequence":"additional","affiliation":[{"name":"British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK"}]}],"member":"1881","published-online":{"date-parts":[[2022,9,30]]},"reference":[{"key":"e_1_3_6_2_1","doi-asserted-by":"publisher","DOI":"10.1016\/0895-9811(92)90059-8"},{"key":"e_1_3_6_3_1","doi-asserted-by":"publisher","DOI":"10.1144\/gsjgs.139.6.0787"},{"key":"e_1_3_6_6_1","doi-asserted-by":"publisher","DOI":"10.1080\/00206814.2019.1655669"},{"key":"e_1_3_6_7_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.gr.2019.10.018"},{"key":"e_1_3_6_8_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.lithos.2021.106013"},{"key":"e_1_3_6_9_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.dib.2021.107042"},{"key":"e_1_3_6_10_1","doi-asserted-by":"publisher","DOI":"10.1080\/00206810902867690"},{"key":"e_1_3_6_11_1","doi-asserted-by":"publisher","DOI":"10.1029\/2019TC005825"},{"key":"e_1_3_6_12_1","doi-asserted-by":"publisher","DOI":"10.1130\/B30820.1"},{"key":"e_1_3_6_13_1","doi-asserted-by":"publisher","DOI":"10.1144\/jgs2014-110"},{"key":"e_1_3_6_14_1","article-title":"Tectonic control on episodic magmatic flare-up events revealed by AMS and U\u2013Pb geochronology on the Antarctic Peninsula","author":"Burton-Johnson A.","unstructured":"Burton-Johnson, A., Riley, T., Harrison, R., Mac Niocaill, M., Muraszko, J. and Rowley, P. in press. 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