Beryllium in Metamorphic Environments (emphasis on aluminous compositions)

Research Article| January 01, 2002 Beryllium in Metamorphic Environments (emphasis on aluminous compositions) Edward S. Grew Edward S. Grew Department of Geological Sciences, University of Maine, 5790 Bryand Center, Orono, Maine 04469, esgrew@maine.edu Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2002) 50 (1): 487–549. https://doi.org/10.2138/rmg.2002.50.12 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 Edward S. Grew; Beryllium in Metamorphic Environments (emphasis on aluminous compositions). Reviews in Mineralogy and Geochemistry 2002;; 50 (1): 487–549. doi: https://doi.org/10.2138/rmg.2002.50.12 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 Beryllium is an element thought to be largely associated with igneous and hydrothermal processes and the world's major economic Be deposits are largely igneous or hydrothermal. However, metamorphic rocks also play a major role in the Be budget of the Earth's crust. Beryllium enrichments in pegmatites and hydrothermal deposits are associated with granitic systems that many geoscientists think are derived from melting of metasedimentary rocks, with metapelites being the most fertile for Be (e.g., London and Evensen, this volume). Consequently, metamorphism plays an important role in the cycling beryllium from sediments to granitic systems. The emphasis of my chapter is... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.