Abstract
Research Article| January 01, 2002 (U-Th)/He Dating of Phosphates: Apatite, Monazite, and Xenotime Kenneth A. Farley; Kenneth A. Farley Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125 Search for other works by this author on: GSW Google Scholar Daniel F. Stockli Daniel F. Stockli Department of Geology, University of Kansas, Lawrence, Kansas 66045 Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2002) 48 (1): 559–577. https://doi.org/10.2138/rmg.2002.48.15 Article history first online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Kenneth A. Farley, Daniel F. Stockli; (U-Th)/He Dating of Phosphates: Apatite, Monazite, and Xenotime. Reviews in Mineralogy and Geochemistry 2002;; 48 (1): 559–577. doi: https://doi.org/10.2138/rmg.2002.48.15 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 common phosphate minerals, apatite Ca5(PO4)3(F,OH,Cl), monazite (Ce,La,Th)PO4, and xenotime YPO4, have found widespread use in geochronology because they incorporate U and Th into their structures. For example, apatite usually has a few tens of ppm of both U and Th, while monazite and xenotime usually have hundreds of ppm to weight percent levels of these elements. As a consequence, these phosphates can be dated using several fundamentally different isotopic techniques. Elsewhere in this volume Harrison et al. describe phosphate dating using ingrowth of radiogenic Pb, the final daughter of... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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