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• W2114972009 abstract "Research Article| April 01, 2007 First application of titanium-in-zircon thermometry to ultrahigh-temperature metamorphism J.A. Baldwin; J.A. Baldwin 1Department of Geosciences, University of Montana, Missoula, Montana 59812, USA Search for other works by this author on: GSW Google Scholar M. Brown; M. Brown 2Laboratory for Crustal Petrology, Department of Geology, University of Maryland, College Park, Maryland 20742, USA Search for other works by this author on: GSW Google Scholar M.D. Schmitz M.D. Schmitz 3Department of Geosciences, Boise State University, Boise, Idaho 83725, USA Search for other works by this author on: GSW Google Scholar Author and Article Information J.A. Baldwin 1Department of Geosciences, University of Montana, Missoula, Montana 59812, USA M. Brown 2Laboratory for Crustal Petrology, Department of Geology, University of Maryland, College Park, Maryland 20742, USA M.D. Schmitz 3Department of Geosciences, Boise State University, Boise, Idaho 83725, USA Publisher: Geological Society of America Received: 11 Aug 2006 Revision Received: 04 Oct 2006 Accepted: 13 Oct 2006 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2007) 35 (4): 295–298. https://doi.org/10.1130/G23285A.1 Article history Received: 11 Aug 2006 Revision Received: 04 Oct 2006 Accepted: 13 Oct 2006 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation J.A. Baldwin, M. Brown, M.D. Schmitz; First application of titanium-in-zircon thermometry to ultrahigh-temperature metamorphism. Geology 2007;; 35 (4): 295–298. doi: https://doi.org/10.1130/G23285A.1 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 Titanium-in-zircon thermometry has been applied to evaluate the temperatures of metamorphism for two ultrahigh-temperature (UHT) granulite localities, the Neoproterozoic Anápolis-Itauçu Complex in central Brazil, and lower crustal xenoliths from the Neo-archean Kaapvaal craton in South Africa. UHT metamorphism in the Anápolis-Itauçu Complex occurred ca. 640 Ma. Ti-in-zircon thermometry on metamorphic zircon yields temperatures of 965–811 °C; a population of late zircon that formed from ilmenite and rutile breakdown records temperatures of ∼780 °C. Maximum temperatures are less than those inferred from quantitative phase equilibria modeling. Based on textural setting (inclusions in peak phases and as matrix grains), these zircons likely record growth during the pro-grade and/or postpeak evolution. In contrast, the Kaapvaal xenoliths record two phases of zircon growth: during UHT metamorphism at 2720–2715 Ma, followed by growth during isobaric cooling in kyanite-bearing leucosomes ca. 2690 Ma. Temperatures recorded by the two phases of growth are 1024–878 °C and 936–839 °C, respectively, suggesting that zircon growth occurred during UHT conditions and continued throughout the postpeak evolution over a 200 °C interval. These examples demonstrate that the Ti-in-zircon thermometer is a powerful new tool with the potential to determine crystallization temperatures of zircon during granulite facies metamorphism, throughout the prograde to postpeak evolution of such terranes. 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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• W2114972009 title "First application of titanium-in-zircon thermometry to ultrahigh-temperature metamorphism" @default.
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