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- W2077893350 abstract "Research Article| January 01, 2002 Beryllium in Silicic Magmas and the Origin of Beryl-Bearing Pegmatites David London; David London School of Geology & Geophysics University of Oklahoma Norman, Oklahoma 73019, dlondon@ou.edu Search for other works by this author on: GSW Google Scholar Joseph M. Evensen Joseph M. Evensen School of Geology & Geophysics University of Oklahoma Norman, Oklahoma 73019, dlondon@ou.edu Search for other works by this author on: GSW Google Scholar Author and Article Information David London School of Geology & Geophysics University of Oklahoma Norman, Oklahoma 73019, dlondon@ou.edu Joseph M. Evensen School of Geology & Geophysics University of Oklahoma Norman, Oklahoma 73019, dlondon@ou.edu Publisher: Mineralogical Society of America First Online: 14 Jul 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2002) 50 (1): 445–486. https://doi.org/10.2138/rmg.2002.50.11 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 David London, Joseph M. Evensen; Beryllium in Silicic Magmas and the Origin of Beryl-Bearing Pegmatites. Reviews in Mineralogy and Geochemistry 2002;; 50 (1): 445–486. doi: https://doi.org/10.2138/rmg.2002.50.11 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 This chapter addresses the portion of the geochemical cycle of beryllium that entails its transfer through the continental crust by the generation and migration of silicic magmas, which will be referred to loosely as granitic but will include all of the textural variants of rocks derived from the granitic bulk compositions. Within the granite system, we will examine the distribution of Be between anatectic melts and residual crystals, and we will track the accumulation of Be in melt via crystal fractionation, culminating in the saturation of pegmatite-forming melts in the mineral beryl. Beryl is unquestionably the most common manifestation of... You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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- W2077893350 date "2002-01-01" @default.
- W2077893350 modified "2023-10-18" @default.
- W2077893350 title "Beryllium in Silicic Magmas and the Origin of Beryl-Bearing Pegmatites" @default.
- W2077893350 cites W140271018 @default.
- W2077893350 cites W1499396558 @default.
- W2077893350 cites W1569655878 @default.
- W2077893350 cites W1623750096 @default.
- W2077893350 cites W1628109531 @default.
- W2077893350 cites W1824760913 @default.
- W2077893350 cites W1963622266 @default.
- W2077893350 cites W1965040265 @default.
- W2077893350 cites W1975221919 @default.
- W2077893350 cites W1978432636 @default.
- W2077893350 cites W1979790829 @default.
- W2077893350 cites W1985040213 @default.
- W2077893350 cites W1986692560 @default.
- W2077893350 cites W1988669121 @default.
- W2077893350 cites W1993307882 @default.
- W2077893350 cites W2000272657 @default.
- W2077893350 cites W2003308803 @default.
- W2077893350 cites W2005475436 @default.
- W2077893350 cites W2013663553 @default.
- W2077893350 cites W2015918891 @default.
- W2077893350 cites W2019751060 @default.
- W2077893350 cites W2036707437 @default.
- W2077893350 cites W2045586119 @default.
- W2077893350 cites W2049635825 @default.
- W2077893350 cites W2051483687 @default.
- W2077893350 cites W2056846507 @default.
- W2077893350 cites W2056971059 @default.
- W2077893350 cites W2064145353 @default.
- W2077893350 cites W2064146655 @default.
- W2077893350 cites W2064697400 @default.
- W2077893350 cites W2066600867 @default.
- W2077893350 cites W2067486513 @default.
- W2077893350 cites W2070341572 @default.
- W2077893350 cites W2073212382 @default.
- W2077893350 cites W2075449021 @default.
- W2077893350 cites W2078180163 @default.
- W2077893350 cites W2080048493 @default.
- W2077893350 cites W2088279173 @default.
- W2077893350 cites W2093564640 @default.
- W2077893350 cites W2093640209 @default.
- W2077893350 cites W2098653297 @default.
- W2077893350 cites W2100499324 @default.
- W2077893350 cites W2103578787 @default.
- W2077893350 cites W2108781293 @default.
- W2077893350 cites W2109088573 @default.
- W2077893350 cites W2112126257 @default.
- W2077893350 cites W2117200354 @default.
- W2077893350 cites W2120848012 @default.
- W2077893350 cites W2126539747 @default.
- W2077893350 cites W2129918057 @default.
- W2077893350 cites W2135785473 @default.
- W2077893350 cites W2135961602 @default.
- W2077893350 cites W2140539610 @default.
- W2077893350 cites W2142994199 @default.
- W2077893350 cites W2153327342 @default.
- W2077893350 cites W2154089632 @default.
- W2077893350 cites W2154241237 @default.
- W2077893350 cites W2155731706 @default.
- W2077893350 cites W2157430657 @default.
- W2077893350 cites W2170091491 @default.
- W2077893350 cites W2172276300 @default.
- W2077893350 cites W2189314351 @default.
- W2077893350 cites W2233670970 @default.
- W2077893350 cites W2257534379 @default.
- W2077893350 cites W2274857742 @default.
- W2077893350 cites W2290828440 @default.
- W2077893350 cites W2312666490 @default.
- W2077893350 cites W2334436772 @default.
- W2077893350 cites W2338158576 @default.
- W2077893350 cites W2343797273 @default.
- W2077893350 cites W2416115622 @default.
- W2077893350 cites W2419513780 @default.
- W2077893350 cites W2460600588 @default.
- W2077893350 cites W2473482373 @default.
- W2077893350 cites W2516084827 @default.
- W2077893350 cites W2559344394 @default.
- W2077893350 cites W2580256240 @default.
- W2077893350 cites W2589038929 @default.
- W2077893350 cites W2601714642 @default.
- W2077893350 cites W2602267356 @default.
- W2077893350 cites W2604065433 @default.
- W2077893350 cites W2792841553 @default.
- W2077893350 cites W2973976400 @default.
- W2077893350 cites W2994277516 @default.
- W2077893350 cites W3120388747 @default.
- W2077893350 cites W3128644006 @default.
- W2077893350 cites W3208508789 @default.
- W2077893350 cites W3215831011 @default.
- W2077893350 cites W86462072 @default.
- W2077893350 cites W2344968519 @default.
- W2077893350 cites W2506962668 @default.