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Research Article| January 02, 2003 Zircon Saturation Thermometry John M. Hanchar; John M. Hanchar Department of Earth and Environmental Sciences, The George Washington University, Washington, DC 20006 Search for other works by this author on: GSW Google Scholar E. Bruce Watson E. Bruce Watson Department of Earth and Environmental Science, Rensselaer Polytechnic Institute, Troy, New York 12180 Search for other works by this author on: GSW Google Scholar Author and Article Information John M. Hanchar Department of Earth and Environmental Sciences, The George Washington University, Washington, DC 20006 E. Bruce Watson Department of Earth and Environmental Science, Rensselaer Polytechnic Institute, Troy, New York 12180 Publisher: Mineralogical Society of America First Online: 03 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2003) 53 (1): 89–112. https://doi.org/10.2113/0530089 Article history First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation John M. Hanchar, E. Bruce Watson; Zircon Saturation Thermometry. Reviews in Mineralogy and Geochemistry 2003;; 53 (1): 89–112. doi: https://doi.org/10.2113/0530089 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 SocietyReviews in Mineralogy and Geochemistry Search Advanced Search The ability of crystalline zircon (ZrSiO4) to incorporate and retain trace element and isotopic information, due to sluggish diffusion, makes it an indispensable tool for geochemists and geochronologists (Valley, this volume; Cherniak and Watson, this volume) in deciphering the Earth's geologic history. The stability of crystalline zircon over long periods of geologic time led researchers to prefer this mineral for geochronology (Heaman and Parrish 1991, Dickin 1995, Davis et al., this volume; Parrish and Noble, this volume). In fact, much of what is known about the timing of major geologic events has been accomplished through... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
Published in: Reviews in Mineralogy and Geochemistry
Volume 53, Issue 1, pp. 89-112
DOI: 10.2113/0530089