{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,1,31]],"date-time":"2026-01-31T00:00:02Z","timestamp":1769817602047,"version":"3.49.0"},"reference-count":90,"publisher":"Geological Society of London","issue":"4","license":[{"start":{"date-parts":[[2014,3,20]],"date-time":"2014-03-20T00:00:00Z","timestamp":1395273600000},"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":[[2014,7]]},"abstract":"<jats:p>\n            Radiometric dating by the\n            <jats:sup>40<\/jats:sup>\n            Ar\u2013\n            <jats:sup>39<\/jats:sup>\n            Ar incremental heating method was carried out on lavas, sills, dykes, and a central intrusion from NE Greenland. Eighteen samples gave acceptable crystallization ages. Lavas of both Lower and Upper Plateau Lava Series gave ages in the range 55.5\u201353.5 Ma and cannot be constrained to better than 56\u201353 Ma. Sills and dykes from Traill \u00d8 to Shannon, with compositions fairly similar to those of the lavas, gave ages of 55.1\u201351.3 Ma, contemporaneous with and slightly younger than the lavas. Alkaline lavas on inland nunataks have ages of 53\u201350 Ma, and the Kap Broer Ruys intrusive centre has an age of 48.7 \u00b1 0.5 Ma. An alkaline sill on Hvalros\u00f8 is much younger at 20.3 \u00b1 0.1 Ma. There are no pre-breakup lavas onshore NE Greenland. We surmise that the hot mantle of the Iceland plume arrived and melted extensively beneath the northern basins only at the time of breakup around 55 Ma. Post-breakup intrusive events in NE Greenland coincided with plate-tectonic events such as reorganization, uplift and opening in the north. The Hvalros\u00f8 sill represents a local small melting event that may be related to coeval opening of the Lena Trough.\n          <\/jats:p>\n          <jats:sec>\n            <jats:title>Supplementary materials:<\/jats:title>\n            <jats:p>\n              Details of the source data, results, and the compositions and locations of the dated samples, 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\/SUP18738\">www.geolsoc.org.uk\/SUP18738<\/jats:ext-link>\n              .\n            <\/jats:p>\n          <\/jats:sec>","DOI":"10.1144\/jgs2013-118","type":"journal-article","created":{"date-parts":[[2014,3,21]],"date-time":"2014-03-21T01:38:02Z","timestamp":1395365882000},"page":"539-553","source":"Crossref","is-referenced-by-count":50,"title":["Eocene to Miocene igneous activity in NE Greenland: northward younging of magmatism along the East Greenland margin"],"prefix":"10.1144","volume":"171","author":[{"given":"Lotte M.","family":"Larsen","sequence":"first","affiliation":[{"name":"Geological Survey of Denmark and Greenland, \u00d8ster Voldgade 10, DK-1350 Copenhagen K, Denmark"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Asger K.","family":"Pedersen","sequence":"additional","affiliation":[{"name":"Geological Survey of Denmark and Greenland, \u00d8ster Voldgade 10, DK-1350 Copenhagen K, Denmark"},{"name":"Natural History Museum of Denmark, \u00d8ster Voldgade 5\u20137, DK-1350 Copenhagen K, Denmark"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Christian","family":"Tegner","sequence":"additional","affiliation":[{"name":"Department of Geoscience, Aarhus University, H\u00f8egh-Guldbergs Gade 2, DK-8000 Aarhus C, Denmark"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Robert A.","family":"Duncan","sequence":"additional","affiliation":[{"name":"College of Earth, Ocean and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA"}],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"1881","published-online":{"date-parts":[[2014,3,20]]},"reference":[{"issue":"5","key":"e_1_3_2_2_1","first-page":"1","volume":"87","author":"Backlund H.G.","year":"1932","unstructured":"Backlund H.G., Malmqvist D. 1932. 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