The Stable Isotope Geochemistry of Copper and Zinc

Research Article| January 01, 2004 The Stable Isotope Geochemistry of Copper and Zinc Francis Albarède Francis Albarède Ecole Normale Supérieure de Lyon, 46 Allée d'Italie, 69007 Lyon, France Search for other works by this author on: GSW Google Scholar Author and Article Information Francis Albarède Ecole Normale Supérieure de Lyon, 46 Allée d'Italie, 69007 Lyon, France Publisher: Mineralogical Society of America First Online: 03 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2004) 55 (1): 409–427. https://doi.org/10.2138/gsrmg.55.1.409 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 Francis Albarède; The Stable Isotope Geochemistry of Copper and Zinc. Reviews in Mineralogy and Geochemistry 2004;; 55 (1): 409–427. doi: https://doi.org/10.2138/gsrmg.55.1.409 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 Copper and zinc are the last two elements of the first row of transition metals (d-block). Interest in these elements arises because they are both strongly chalcophile and, thanks to a rich coordination chemistry, participate in a large number of important biological compounds and reactions. Copper has two isotopes, 63Cu and 65Cu with respective abundances of 69.174% and 30.826% in the reference metal SRM-NIST 976 (Shields et al. 1964). Zn has fi ve stable isotopes 64Zn, 66Zn, 67Zn, 68Zn, and 70Zn with average natural abundances of 48.63, 27.90, 4.10, 18.75, and... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.