Item talk:Q254240
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "U-Th-Pb zircon ages of some Keweenawan Supergroup rocks from the south shore of Lake Superior", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70019942", "url": "https://pubs.usgs.gov/publication/70019942" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70019942 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1139/e17-044", "url": "https://doi.org/10.1139/e17-044" }, { "@type": "PropertyValue", "propertyID": "ISSN", "value": "00084077" } ], "journal": { "@type": "Periodical", "name": "Canadian Journal of Earth Sciences", "volumeNumber": "34", "issueNumber": "4" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Canadian Journal of Earth Sciences" } ], "datePublished": "1997", "dateModified": "2023-09-20", "abstract": "New single-crystal zircon U\u2013Th\u2013Pb ages for plutonic and rhyolitic Keweenawan Supergroup rocks from the south shore of Lake Superior provide geochronological constraints on magmatic evolution associated with the 1.1\u2002Ga Midcontinent rift. Analyses of a granophyric phase of the Mineral Lake intrusion and the Mellen granite, both parts of the Mellen Intrusive Complex, and a laterally extensive rhyolite from the top of the Kallander Creek Volcanics have weighted average\u00a0207Pb/206Pb ages of 1102.0\u2002\u00b1\u20022.8\u2002Ma (N\u2002=\u20022), 1100.9\u2002\u00b1\u20021.4\u2002Ma (N\u2002=\u20025), and 1098.8\u2002\u00b1\u20021.9\u2002Ma (N\u2002=\u20024), respectively. Analyses of a pyroclastic rhyolite flow at the top of the Porcupine Volcanics result in variable\u00a0207Pb/206Pb ages that range from 1080 to 1137\u2002Ma. This rhyolite exhibits a continuum between morphologically complex and simpler prismatic zircon crystals, the latter yielding concordant analyses having a weighted average\u00a0207Pb/206Pb age of 1093.6\u2002\u00b1\u20021.8 Ma (N\u2002=\u20022). Four prismatic zircons from an aphyric rhyolite of the Chengwatana Volcanics in the Ashland syncline form a linear array intersecting concordia at 1094.6\u2002\u00b1\u20022.1\u2002Ma (MSWD\u2002=\u20021.3). Another presumed Chengwatana rhyolite recovered from drill core intersecting the Hudson\u2013Afton horst in southeast Minnesota yielded only ~20 morphologically indistinguishable zircons. Six analyses give\u00a0207Pb/206Pb ages ranging from 1112 to 1136\u2002Ma, including one analysis with a virtually concordant age of 1130\u2002Ma. This age, however, is considerably older than that obtained for the Chengwatana Volcanics in the Ashland syncline or any other precisely dated rock from the Midcontinent rift.", "description": "13 p.", "publisher": { "@type": "Organization", "name": "Canadian Science Publishing" }, "author": [ { "@type": "Person", "name": "Zartman, R. E.", "givenName": "R. E.", "familyName": "Zartman" }, { "@type": "Person", "name": "Cannon, W. F.", "givenName": "W. 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