Oxygen Isotopes in Mantle and Crustal Magmas as Revealed by Single Crystal Analysis

Research Article| January 01, 2008 Oxygen Isotopes in Mantle and Crustal Magmas as Revealed by Single Crystal Analysis Ilya Bindeman Ilya Bindeman Department of Geological Sciences, University of Oregon, Eugene, Oregon, 97403-1272, U.S.A., bindeman@uoregon.edu Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2008) 69 (1): 445–478. https://doi.org/10.2138/rmg.2008.69.12 Article history first online: 13 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Ilya Bindeman; Oxygen Isotopes in Mantle and Crustal Magmas as Revealed by Single Crystal Analysis. Reviews in Mineralogy and Geochemistry 2008;; 69 (1): 445–478. doi: https://doi.org/10.2138/rmg.2008.69.12 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 Oxygen is the most abundant element in the Earth’s crust, mantle, and fluids and therefore its isotopic composition provides robust constraints on magma genesis. Application of oxygen isotope geochemistry to volcanology and igneous petrology provides a much needed foundation for radiogenic isotope and trace element approaches. Since isotope fractionations at high temperature are small, there is a demand for high analytical precision in order to recognize and interpret small (tenths of permil) variations in isotopic composition. Recently improved analytical techniques involving lasers and ion microprobes, and reduction in sample and spot size, has painted a picture of isotope complexity on… You do not have access to this content, please speak to your institutional administrator if you feel you should have access.