{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,4,2]],"date-time":"2026-04-02T10:11:01Z","timestamp":1775124661324,"version":"3.50.1"},"reference-count":197,"publisher":"Geological Society of London","issue":"1","license":[{"start":{"date-parts":[[2020,1,1]],"date-time":"2020-01-01T00:00:00Z","timestamp":1577836800000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"funder":[{"DOI":"10.13039\/501100001824","name":"Grantov\u00e1 Agentura \u010cesk\u00e9 Republiky","doi-asserted-by":"crossref","award":["18-24378S"],"award-info":[{"award-number":["18-24378S"]}],"id":[{"id":"10.13039\/501100001824","id-type":"DOI","asserted-by":"crossref"}]}],"content-domain":{"domain":["www.lyellcollection.org"],"crossmark-restriction":true},"short-container-title":["SP"],"published-print":{"date-parts":[[2020,1]]},"abstract":"<jats:title>Abstract<\/jats:title>\n          <jats:p>\n            Granites (\n            <jats:italic>sensu lato<\/jats:italic>\n            ) come in many types and flavours, defining distinct magmatic series\/suites\/types. A good classification not only gives generally accepted and understandable names to similar rocks but also links the bulk chemical composition to the stoichiometry of the constituent minerals and, potentially, also to the likely source, magmatic evolution and tectonic setting.\n          <\/jats:p>\n          <jats:p>\n            The \u2018ideal\u2019 granitoid classification should be based on chemical criteria amenable to an objective treatment. Statistical analysis helps to identify the most discriminant variables. The key properties are (1) acidity\/maficity, (2) alkalinity (balance of Na + K v. Ca), (3) aluminosity (balance of Al v. Ca, Na and K), (4) Fe\/Mg balance and (5) Na\/K balance and K contents at the given SiO\n            <jats:sub>2<\/jats:sub>\n            level. These are used by successful classifications, e.g. the I\/S dichotomy is based mainly on aluminosity, while the Frost\n            <jats:italic>et al.<\/jats:italic>\n            (2001; \u2018A geochemical classification for granitic rocks',\n            <jats:italic>Journal of Petrology<\/jats:italic>\n            ,\n            <jats:bold>42<\/jats:bold>\n            , 2033\u20132048,\n            <jats:uri xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" xlink:href=\"https:\/\/doi.org\/10.1093\/petrology\/42.11.2033\">https:\/\/doi.org\/10.1093\/petrology\/42.11.2033<\/jats:uri>\n            ) classification includes all but Na\/K. Even though it is commonplace to use weight percentages of oxides, we suggest that a better strategy is to employ simple atomic parameters (e.g. millications-based) that can be directly linked to modal proportions and compositions\/crystal structure of individual rock-forming minerals. This facilitates a petrological interpretation, which, in turn, can be related to petrogenesis and, ultimately, to likely tectonic setting(s).\n          <\/jats:p>","DOI":"10.1144\/sp491-2019-138","type":"journal-article","created":{"date-parts":[[2019,12,6]],"date-time":"2019-12-06T15:34:11Z","timestamp":1575646451000},"page":"9-51","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":74,"title":["Chemical variation, modal composition and classification of granitoids"],"prefix":"10.1144","volume":"491","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-2981-4046","authenticated-orcid":false,"given":"Bernard","family":"Bonin","sequence":"first","affiliation":[{"name":"UMR 8148 \u2018GEOPS\u2019, Universit\u00e9 Paris-Sud, CNRS, Universit\u00e9 Paris-Saclay, B\u00e2timent 504, Rue du Belv\u00e9d\u00e8re, F-91405 Orsay Cedex, France"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-6581-9207","authenticated-orcid":false,"given":"Vojt\u011bch","family":"Janou\u0161ek","sequence":"additional","affiliation":[{"name":"Czech Geological Survey, Kl\u00e1rov 3, 118 21 Prague 1, Czech Republic"},{"name":"Institute of Petrology and Structural Geology, Faculty of Science, Charles University, Albertov 6, 128 43 Prague 2, Czech Republic"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-0065-2442","authenticated-orcid":false,"given":"Jean-Fran\u00e7ois","family":"Moyen","sequence":"additional","affiliation":[{"name":"Laboratoire Magmas et Volcans, UJM-UCA-CNRS-IRD, Universit\u00e9 de Lyon, 23 Rue du Dr Paul Michelon, 42023 Saint Etienne, France"}]}],"member":"1881","published-online":{"date-parts":[[2020,2,11]]},"reference":[{"key":"e_1_3_4_2_1","doi-asserted-by":"publisher","DOI":"10.1007\/978-94-009-4109-0"},{"key":"e_1_3_4_3_1","doi-asserted-by":"publisher","DOI":"10.1016\/0098-3004(77)90007-3"},{"key":"e_1_3_4_4_1","doi-asserted-by":"publisher","DOI":"10.1007\/s00410-008-0351-8"},{"key":"e_1_3_4_5_1","doi-asserted-by":"publisher","DOI":"10.1515\/9781501508486-005"},{"key":"e_1_3_4_6_1","doi-asserted-by":"publisher","DOI":"10.1016\/0377-0273(87)90033-3"},{"key":"e_1_3_4_7_1","doi-asserted-by":"publisher","DOI":"10.1093\/petrology\/44.5.929"},{"key":"e_1_3_4_8_1","doi-asserted-by":"publisher","DOI":"10.1007\/BF00385783"},{"key":"e_1_3_4_9_1","doi-asserted-by":"publisher","DOI":"10.1002\/gj.3350250306"},{"key":"e_1_3_4_10_1","doi-asserted-by":"publisher","DOI":"10.1130\/0091-7613(1996)024<0295:GOTTMT>2.3.CO;2"},{"key":"e_1_3_4_11_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0024-4937(98)00085-1"},{"key":"e_1_3_4_12_1","doi-asserted-by":"publisher","DOI":"10.1029\/JB086iB11p10131"},{"key":"e_1_3_4_13_1","doi-asserted-by":"publisher","DOI":"10.2138\/am-2017-6063"},{"key":"e_1_3_4_14_1","doi-asserted-by":"publisher","DOI":"10.1016\/0009-2541(85)90034-8"},{"key":"e_1_3_4_15_1","doi-asserted-by":"publisher","DOI":"10.1130\/0091-7613(1977)5<252:ICOGRA>2.0.CO;2"},{"key":"e_1_3_4_16_1","first-page":"49","article-title":"Use of the chemical TAS diagram (total alkali\u2013silica) for classification of plutonic rocks: problems and suggestions","volume":"14","author":"Bellieni G.","year":"1995","unstructured":"BellieniG., VisentinJ. & ZanettinB. 1995. 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