Uranium-series Crystal Ages

Research Article| January 01, 2008 Uranium-series Crystal Ages Kari M. Cooper; Kari M. Cooper Department of Geology, University of California, Davis, California, 95616, U.S.A., kmcooper@geology.ucdavis.edu Search for other works by this author on: GSW Google Scholar Mary R. Reid Mary R. Reid Department of Geology, Northern Arizona University, Flagstaff, Arizona, 86011, U.S.A., mary.reid@nau.edu Search for other works by this author on: GSW Google Scholar Author and Article Information Kari M. Cooper Department of Geology, University of California, Davis, California, 95616, U.S.A., kmcooper@geology.ucdavis.edu Mary R. Reid Department of Geology, Northern Arizona University, Flagstaff, Arizona, 86011, U.S.A., mary.reid@nau.edu Publisher: Mineralogical Society of America First Online: 13 Jul 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2008) 69 (1): 479–544. https://doi.org/10.2138/rmg.2008.69.13 Article history First Online: 13 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Kari M. Cooper, Mary R. Reid; Uranium-series Crystal Ages. Reviews in Mineralogy and Geochemistry 2008;; 69 (1): 479–544. doi: https://doi.org/10.2138/rmg.2008.69.13 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 As the collected papers in this volume aptly demonstrate, chemical and textural records contained within crystals have become increasingly useful tools for understanding the evolution of magmatic systems. An essential component of studies of the dynamics of magmatic systems is the ability to place the thermal, physical, and compositional evolution of magmas in a temporal context. Studies of the kinetics of crystal growth and reaction, and of diffusive re-equilibration of crystals and melts, can provide information about the duration of magmatic processes such as magma ascent (Rutherford 2008), crystal growth (Hammer 2008), and residence of crystals... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.