Kinetic Fractionation of Non-Traditional Stable Isotopes by Diffusion and Crystal Growth Reactions

Research Article| January 01, 2017 Kinetic Fractionation of Non-Traditional Stable Isotopes by Diffusion and Crystal Growth Reactions James M. Watkins; James M. Watkins Department of Geological Sciences University of Oregon Eugene, OR USA, watkins4@uoregon.edu Search for other works by this author on: GSW Google Scholar Donald J. DePaolo; Donald J. DePaolo Earth Sciences Division Lawrence Berkeley National Laboratory Berkeley, CA USA, and Department of Earth and Planetary Science University of California Berkeley, CA USA, DJDepaolo@lbl.gov Search for other works by this author on: GSW Google Scholar E. Bruce Watson E. Bruce Watson Department of Geology Rensselaer Polytechnic Institute Troy, NY USA, watsoe@rpi.edu Search for other works by this author on: GSW Google Scholar Author and Article Information James M. Watkins Department of Geological Sciences University of Oregon Eugene, OR USA, watkins4@uoregon.edu Donald J. DePaolo Earth Sciences Division Lawrence Berkeley National Laboratory Berkeley, CA USA, and Department of Earth and Planetary Science University of California Berkeley, CA USA, DJDepaolo@lbl.gov E. Bruce Watson Department of Geology Rensselaer Polytechnic Institute Troy, NY USA, watsoe@rpi.edu Publisher: Mineralogical Society of America First Online: 14 Jul 2017 © 2017 Mineralogical Society of America Reviews in Mineralogy and Geochemistry (2017) 82 (1): 85–125. https://doi.org/10.2138/rmg.2017.82.4 Article history First Online: 14 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation James M. Watkins, Donald J. DePaolo, E. Bruce Watson; Kinetic Fractionation of Non-Traditional Stable Isotopes by Diffusion and Crystal Growth Reactions. Reviews in Mineralogy and Geochemistry 2017;; 82 (1): 85–125. doi: https://doi.org/10.2138/rmg.2017.82.4 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 Natural variations in the isotopic composition of some 50 chemical elements are now being used in geochemistry for studying transport processes, estimating temperature, reconstructing ocean chemistry, identifying biological signatures, and classifying planets and meteorites. Within the past decade, there has been growing interest in measuring isotopic variations in a wider variety of elements, and improved techniques make it possible to measure very small effects. Many of the observations have raised questions concerning when and where the attainment of equilibrium is a valid assumption. In situations where the distribution of isotopes within and among phases is not representative of the equilibrium... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.