Bowling Green State University ScholarWorks@BGSU Earth, Environment, and Society Faculty Publications School of Earth, Environment and Society 2010 Oxygen and Hydrogen Diffusion In Minerals John Richard Farver Bowling Green State University,
[email protected] Follow this and additional works at: https://scholarworks.bgsu.edu/sees_pub Part of the Earth Sciences Commons Repository Citation Farver, John Richard, "Oxygen and Hydrogen Diffusion In Minerals" (2010). Earth, Environment, and Society Faculty Publications. 2. https://scholarworks.bgsu.edu/sees_pub/2 This Article is brought to you for free and open access by the School of Earth, Environment and Society at ScholarWorks@BGSU. It has been accepted for inclusion in Earth, Environment, and Society Faculty Publications by an authorized administrator of ScholarWorks@BGSU. Reviews in Mineralogy & Geochemistry Vol. 72 pp. 447-507, 2010 10 Copyright © Mineralogical Society of America Oxygen and Hydrogen Diffusion in Minerals John R. Farver Department of Geology Bowling Green State University Bowling Green, Ohio 43403, U.S.A.
[email protected] INTRODUCTION This chapter provides a summary and review of experimentally determined oxygen and hydrogen volume diffusion in minerals. A very extensive and detailed review of stable isotope exchange processes including oxygen and hydrogen volume diffusion can be found in Cole and Chakraborty (2001) and a detailed review of hydrogen diffusion in minerals, especially nominally anhydrous minerals, can be found in Ingrin and Blanchard (2006). In addition, a detailed review of oxygen and hydrogen diffusion in silicate melts is provided by Zhang and Ni (2010), and oxygen and hydrogen diffusion rates can also be found in the chapters, in this volume, on specific minerals and mineral groups (e.g., Van Orman and Crispin 2010; Cherniak 2010).