Non-pegmatitic Deposits of Beryllium: Mineralogy, Geology, Phase Equilibria and Origin

Research Article| January 01, 2002 Non-pegmatitic Deposits of Beryllium: Mineralogy, Geology, Phase Equilibria and Origin Mark D. Barton; Mark D. Barton Center for Mineral Resources, Department of Geosciences, University of Arizona, Tucson, Arizona 85721, barton@geo.arizona.edu Search for other works by this author on: GSW Google Scholar Steven Young Steven Young Center for Mineral Resources, Department of Geosciences, University of Arizona, Tucson, Arizona 85721, barton@geo.arizona.edu Search for other works by this author on: GSW Google Scholar Author and Article Information Mark D. Barton Center for Mineral Resources, Department of Geosciences, University of Arizona, Tucson, Arizona 85721, barton@geo.arizona.edu Steven Young Center for Mineral Resources, Department of Geosciences, University of Arizona, Tucson, Arizona 85721, barton@geo.arizona.edu Publisher: Mineralogical Society of America First Online: 14 Jul 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2002) 50 (1): 591–691. https://doi.org/10.2138/rmg.2002.50.14 Article history First Online: 14 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Mark D. Barton, Steven Young; Non-pegmatitic Deposits of Beryllium: Mineralogy, Geology, Phase Equilibria and Origin. Reviews in Mineralogy and Geochemistry 2002;; 50 (1): 591–691. doi: https://doi.org/10.2138/rmg.2002.50.14 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 Non-pegmatitic occurrences of Be minerals constitute a diverse set of geologic environments of considerable mineralogical and petrological interest; they currently provide the majority of the world's Be ore and emeralds and they contain the greatest resource of these commodities. Of the approximately 100 Be minerals known (see Chapter 1 by Grew; Appendix A1), most occur in hydrothermal deposits or non-pegmatitic igneous rocks, where their distribution varies systematically with the setting and origin (Table 11, Fig. 11). Beryllium minerals are best known from geologic systems associated with felsic magmatism. They also occur in a variety... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.