{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,8,10]],"date-time":"2026-08-10T01:25:40Z","timestamp":1786325140010,"version":"3.56.0"},"reference-count":127,"publisher":"Mineralogical Association of Canada","issue":"2","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":[],"published-print":{"date-parts":[[2022,3,1]]},"abstract":"<jats:title>ABSTRACT<\/jats:title><jats:p>The current classification of granitic pegmatites, originally introduced by \u010cern\u00fd (1991a), has been the accepted system for grouping pegmatites of diverse mineralogy and chemistry for nearly three decades. Despite its general acceptance, several issues have been highlighted (M\u00fcller et al. 2022) which have imposed some limitations on its use and therefore necessitated the need to reevaluate its methodology. A new classification for granitic pegmatites is proposed in an attempt to be more inclusive of pegmatite types omitted in previous classification schemes. The new approach utilizes a more comprehensive suite of accessory minerals and defines three pegmatite groups which are genetically related to granite plutons and the anatexis of metaigneous and metasedimentary protoliths. Pegmatites belonging to Groups 1 and 2 are generated from the residual melts of S-, A-, and I-type granite magmatism (RGM) as well as being direct products of anatexis (DPA), whereas Group 3 pegmatites are only derived by anatexis.<\/jats:p>","DOI":"10.3749\/canmin.1800006","type":"journal-article","created":{"date-parts":[[2022,3,29]],"date-time":"2022-03-29T22:42:39Z","timestamp":1648593759000},"page":"229-248","source":"Crossref","is-referenced-by-count":109,"title":["A proposed new mineralogical classification system for granitic pegmatites"],"prefix":"10.3749","volume":"60","author":[{"given":"Michael A.","family":"Wise","sequence":"first","affiliation":[{"name":"Department of Mineral Sciences, National Museum of Natural History, Smithsonian Institution, 10th St. & Constitution Ave., NW, Washington, D.C. 20560, USA"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Axel","family":"M\u00fcller","sequence":"additional","affiliation":[{"name":"Natural History Museum, P.O. 1172 Blindern, N-0318 Oslo, Norway"},{"name":"Natural History Museum, Cromwell Road, London SW7 5BD, UK"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"William B.","family":"Simmons","sequence":"additional","affiliation":[{"name":"MP2 Research Group, Maine Mineral and Gem Museum, P.O. Box 500, 99 Main Street, Maine 04217, USA"}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"2062","published-online":{"date-parts":[[2022,3,29]]},"reference":[{"key":"2022032919514555800_i1499-1276-60-2-229-Antunes1","doi-asserted-by":"crossref","unstructured":"Antunes, I.M.H.R., Neiva, A.M.R., Ramos, J.M.F., Silva, P.B., Silva, M.M.V.G., & Corfu,F. (2013) Petrogenetic links between lepidolite-subtype aplite-pegmatite, aplite veins and associated granites at Segura (central Portugal). Geochemistry73, 323\u2013 341.","DOI":"10.1016\/j.chemer.2012.12.003"},{"key":"2022032919514555800_i1499-1276-60-2-229-Barros1","doi-asserted-by":"crossref","unstructured":"Barros, R. & Menuge,J.F. (2016) The origin of spodumene pegmatites associated with the Leinster Granite in southeast Ireland. 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