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• W2022341298 abstract "Research Article| April 01, 2003 Intermittent 1630–1220 Ma magmatism in central Mazatzal province: New geochronologic piercing points and some tectonic implications O. Tapani Rämö; O. Tapani Rämö 1Department of Geology, University of Helsinki, P.O. Box 64, FIN-00014, Finland Search for other works by this author on: GSW Google Scholar Virginia T. McLemore; Virginia T. McLemore 2New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, Socorro, New Mexico 87801, USA Search for other works by this author on: GSW Google Scholar Michael A. Hamilton; Michael A. Hamilton 3J.C. Roddick Ion Microprobe (SHRIMP II) Laboratory, Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario K1A 0E8, Canada Search for other works by this author on: GSW Google Scholar Paula J. Kosunen; Paula J. Kosunen 4Department of Geology, University of Helsinki, P.O. Box 64, FIN-00014, Finland Search for other works by this author on: GSW Google Scholar Matt Heizler; Matt Heizler 5New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, Socorro, New Mexico 87801, USA Search for other works by this author on: GSW Google Scholar Ilmari Haapala Ilmari Haapala 6Department of Geology, University of Helsinki, P.O. Box 64, FIN-00014, Finland Search for other works by this author on: GSW Google Scholar Author and Article Information O. Tapani Rämö 1Department of Geology, University of Helsinki, P.O. Box 64, FIN-00014, Finland Virginia T. McLemore 2New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, Socorro, New Mexico 87801, USA Michael A. Hamilton 3J.C. Roddick Ion Microprobe (SHRIMP II) Laboratory, Geological Survey of Canada, 601 Booth Street, Ottawa, Ontario K1A 0E8, Canada Paula J. Kosunen 4Department of Geology, University of Helsinki, P.O. Box 64, FIN-00014, Finland Matt Heizler 5New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, Socorro, New Mexico 87801, USA Ilmari Haapala 6Department of Geology, University of Helsinki, P.O. Box 64, FIN-00014, Finland Publisher: Geological Society of America Received: 28 Sep 2002 Revision Received: 17 Dec 2002 Accepted: 20 Dec 2002 First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2003) 31 (4): 335–338. https://doi.org/10.1130/0091-7613(2003)031<0335:IMMICM>2.0.CO;2 Article history Received: 28 Sep 2002 Revision Received: 17 Dec 2002 Accepted: 20 Dec 2002 First Online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation O. Tapani Rämö, Virginia T. McLemore, Michael A. Hamilton, Paula J. Kosunen, Matt Heizler, Ilmari Haapala; Intermittent 1630–1220 Ma magmatism in central Mazatzal province: New geochronologic piercing points and some tectonic implications. Geology 2003;; 31 (4): 335–338. doi: https://doi.org/10.1130/0091-7613(2003)031<0335:IMMICM>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract The northern Burro Mountains in southwestern New Mexico reveal three distinct, intimately juxtaposed Mesoproterozoic magmatic suites in southern Laurentia. At 1633 Ma, the newly formed Mazatzal crust was intruded by tholeiitic diabase with a depleted-mantle–type Nd isotope composition but with enriched incompatible trace element abundances. A potassic granite-minette suite was emplaced ca. 1460 Ma, and a tholeiitic A-type granite-anorthosite suite intruded ca. 1225–1220 Ma. The diabase-minette-anorthosite sequence and the associated silicic rocks record dominantly juvenile additions to the cratonic margin and imply subcontinental enrichment events ca. 1650 Ma (accretion), prior to 1460 Ma (potassic metasomatism), and ca. 1220 Ma (magmatic underplating). The latter two may have been controlled by a major transcurrent structure along the south margin of Laurentia. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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