Triple Oxygen Isotope Variations in Earth’s Crust

Research Article| January 01, 2021 Triple Oxygen Isotope Variations in Earth's Crust Daniel Herwartz Daniel Herwartz Institut für Geologie und Mineralogie, Universität zu Köln, Zülpicher Str. 49b, 50674 Cologne, Germany * E-mail: d.herwartz@uni-koeln.de Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2021) 86 (1): 291–322. https://doi.org/10.2138/rmg.2021.86.09 Article history first online: 04 Jan 2021 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Daniel Herwartz; Triple Oxygen Isotope Variations in Earth's Crust. Reviews in Mineralogy and Geochemistry 2021;; 86 (1): 291–322. doi: https://doi.org/10.2138/rmg.2021.86.09 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 Analyzing classic 18O/16O ratios in solids, liquids and gases has proven useful in almost every branch of earth science. As reviewed in this book, additional 17O analysis generally help to better constrain the underlying fractionation mechanisms providing a more solid basis to quantify geologic processes. Mass independent fractionation (MIF) effects known from meteorites and atmospheric gases (Clayton et al. 1973; Thiemens and Heidenreich 1983; Thiemens and Lin 2021, this volume; Brinjikji and Lyons 2021, this volume) generate large 17O anomalies (expressed as ∆17O) that can be transferred to... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.