Diffusion in Accessory Minerals: Zircon, Titanite, Apatite, Monazite and Xenotime

Abstract

Research Article| January 01, 2010 Diffusion in Accessory Minerals: Zircon, Titanite, Apatite, Monazite and Xenotime D.J. Cherniak D.J. Cherniak Department of Earth & Environmental Sciences, Rensselaer Polytechnic Institute, Troy, New York 12180, U.S.A., chernd@rpi.edu Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2010) 72 (1): 827–869. https://doi.org/10.2138/rmg.2010.72.18 Article history first online: 09 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 D.J. Cherniak; Diffusion in Accessory Minerals: Zircon, Titanite, Apatite, Monazite and Xenotime. Reviews in Mineralogy and Geochemistry 2010;; 72 (1): 827–869. doi: https://doi.org/10.2138/rmg.2010.72.18 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 In this chapter, an overview of the findings to date from laboratory measurements of diffusion of cations in the accessory mineral phases zircon, monazite, apatite, titanite (sphene) and xenotime is presented. These minerals differ widely from one another in structure and composition, but share some common characteristics. While they are generally low in modal abundance, they tend to incorporate elements that are important tracers of geochemical processes (e.g., the rare earth and high-field strength elements) as well as U and/or Th, which make them valuable as geochronometers. Two other phases commonly considered "accessory," rutile and baddeleyite, are discussed in other... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.