See felsic on Wiktionary
{ "etymology_templates": [ { "args": { "1": "en", "2": "feldspar", "3": "silica" }, "expansion": "Blend of feldspar + silica", "name": "blend" }, { "args": { "1": "en", "2": "", "3": "ic" }, "expansion": "+ -ic", "name": "suf" } ], "etymology_text": "Blend of feldspar + silica, + -ic.", "forms": [ { "form": "more felsic", "tags": [ "comparative" ] }, { "form": "most felsic", "tags": [ "superlative" ] } ], "head_templates": [ { "args": {}, "expansion": "felsic (comparative more felsic, superlative most felsic)", "name": "en-adj" } ], "lang": "English", "lang_code": "en", "pos": "adj", "senses": [ { "categories": [ { "kind": "topical", "langcode": "en", "name": "Petrology", "orig": "en:Petrology", "parents": [ "Geology", "Earth sciences", "Sciences", "All topics", "Fundamental" ], "source": "w" }, { "_dis": "57 43", "kind": "other", "name": "English blends", "parents": [], "source": "w+disamb" }, { "_dis": "54 46", "kind": "other", "name": "English entries with incorrect language header", "parents": [ "Entries with incorrect language header", "Entry maintenance" ], "source": "w+disamb" }, { "_dis": "55 45", "kind": "other", "name": "English terms suffixed with -ic", "parents": [], "source": "w+disamb" }, { "_dis": "51 49", "kind": "other", "name": "Pages with 1 entry", "parents": [], "source": "w+disamb" }, { "_dis": "48 52", "kind": "other", "name": "Pages with entries", "parents": [], "source": "w+disamb" }, { "_dis": "64 36", "kind": "topical", "langcode": "en", "name": "Rocks", "orig": "en:Rocks", "parents": [ "Geology", "Natural materials", "Earth sciences", "Materials", "Nature", "Sciences", "Manufacturing", "All topics", "Human activity", "Fundamental", "Human behaviour", "Human" ], "source": "w+disamb" } ], "derived": [ { "word": "felsification" }, { "word": "nonfelsic" } ], "examples": [ { "text": "Coordinate term: mafic" }, { "ref": "1954, J. C. Olson, D. R. Shawe, L. C. Pray, W. N. Sharp, Rare-Earth Mineral Deposits of the Mountain Pass District, San Bernadino County, California, U.S. Geological Survey, Professional Paper 261, page 22:", "text": "Much of the southern half of the southeastern body is a mafic syenite, slightly more felsic than the shonkinite.", "type": "quote" }, { "ref": "1983, Paul C. Bateman, “A summary of critical relations in the central part of Sierra Nevada batholith, California, U.S.A.”, in J. A. Roddick, editor, Circum-Pacific Plutonic Terranes, Geological Society of America, Memoir 159, page 241:", "text": "Within comagmatic suites, successively younger granitoids are commonly, but not invariably, more felsic, representing progressively lower temperature mineral assemblages.", "type": "quote" }, { "ref": "1992, David C. Champion, Bruce W. Chappell, “Petrogenesis of felsic I-type granites: an example from northern Queensland”, in P. E. Brown, B. W. Chappell, editor, The Second Hutton Symposium on the Origin of Granites and Related Rocks, Geological Society of America, Special Paper 272, page 115:", "text": "The Claret Creek Supersuite granites are a little more felsic (65-77% SiO₂), and are chemically distinctive, having higher Al₂O₃, CaO, Na₂O and Sr, and lower K₂O, Rb, Th and U than the granites of the Almaden Supersuite.", "type": "quote" } ], "glosses": [ "Enriched in minerals predominantly composed of the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium." ], "id": "en-felsic-en-adj-tdFxHYTn", "links": [ [ "petrology", "petrology" ] ], "raw_glosses": [ "(petrology) Enriched in minerals predominantly composed of the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium." ], "related": [ { "word": "felsite" } ], "synonyms": [ { "word": "acidic" }, { "word": "sialic" }, { "word": "silicic" } ], "topics": [ "geography", "geology", "natural-sciences", "petrology" ] } ], "sounds": [ { "audio": "LL-Q1860 (eng)-Vealhurl-felsic.wav", "mp3_url": "https://upload.wikimedia.org/wikipedia/commons/transcoded/8/81/LL-Q1860_%28eng%29-Vealhurl-felsic.wav/LL-Q1860_%28eng%29-Vealhurl-felsic.wav.mp3", "ogg_url": "https://upload.wikimedia.org/wikipedia/commons/transcoded/8/81/LL-Q1860_%28eng%29-Vealhurl-felsic.wav/LL-Q1860_%28eng%29-Vealhurl-felsic.wav.ogg" } ], "word": "felsic" } { "etymology_templates": [ { "args": { "1": "en", "2": "feldspar", "3": "silica" }, "expansion": "Blend of feldspar + silica", "name": "blend" }, { "args": { "1": "en", "2": "", "3": "ic" }, "expansion": "+ -ic", "name": "suf" } ], "etymology_text": "Blend of feldspar + silica, + -ic.", "forms": [ { "form": "felsics", "tags": [ "plural" ] } ], "head_templates": [ { "args": {}, "expansion": "felsic (plural felsics)", "name": "en-noun" } ], "lang": "English", "lang_code": "en", "pos": "noun", "senses": [ { "categories": [ { "_dis": "54 46", "kind": "other", "name": "English entries with incorrect language header", "parents": [ "Entries with incorrect language header", "Entry maintenance" ], "source": "w+disamb" }, { "_dis": "55 45", "kind": "other", "name": "English terms suffixed with -ic", "parents": [], "source": "w+disamb" }, { "_dis": "51 49", "kind": "other", "name": "Pages with 1 entry", "parents": [], "source": "w+disamb" }, { "_dis": "48 52", "kind": "other", "name": "Pages with entries", "parents": [], "source": "w+disamb" } ], "examples": [ { "ref": "1953, R. C. Emmons, “Petrogeny of the Syenites and Nepheline Syenites of Central Wisconsin”, in R. C. Emmons, editor, Selected Petrogenic Relationships of Plagioclase, Geological Society of America, Memoir 52, page 80:", "text": "The central part of this nepheline syenite is very white felsics with black mafics in it. The entire area contains many nepheline-bearing dike rocks, but almost all are gray or pink or even red due to the color in the felsics.", "type": "quote" }, { "ref": "1992, T. E. Smith, chapter 1, in K. C. Condie, editor, Proterozoic Crustal Evolution, Elsevier, page 35:", "text": "There are also calcalkaline felsics that have highly enriched LREE^([light rare-earth element]) patterns with lower overall abundances.", "type": "quote" } ], "glosses": [ "A rock with such properties." ], "id": "en-felsic-en-noun-smHsDz7V" } ], "sounds": [ { "audio": "LL-Q1860 (eng)-Vealhurl-felsic.wav", "mp3_url": "https://upload.wikimedia.org/wikipedia/commons/transcoded/8/81/LL-Q1860_%28eng%29-Vealhurl-felsic.wav/LL-Q1860_%28eng%29-Vealhurl-felsic.wav.mp3", "ogg_url": "https://upload.wikimedia.org/wikipedia/commons/transcoded/8/81/LL-Q1860_%28eng%29-Vealhurl-felsic.wav/LL-Q1860_%28eng%29-Vealhurl-felsic.wav.ogg" } ], "word": "felsic" }
{ "categories": [ "English adjectives", "English blends", "English countable nouns", "English entries with incorrect language header", "English lemmas", "English nouns", "English terms suffixed with -ic", "Pages with 1 entry", "Pages with entries", "en:Rocks" ], "derived": [ { "word": "felsification" }, { "word": "nonfelsic" } ], "etymology_templates": [ { "args": { "1": "en", "2": "feldspar", "3": "silica" }, "expansion": "Blend of feldspar + silica", "name": "blend" }, { "args": { "1": "en", "2": "", "3": "ic" }, "expansion": "+ -ic", "name": "suf" } ], "etymology_text": "Blend of feldspar + silica, + -ic.", "forms": [ { "form": "more felsic", "tags": [ "comparative" ] }, { "form": "most felsic", "tags": [ "superlative" ] } ], "head_templates": [ { "args": {}, "expansion": "felsic (comparative more felsic, superlative most felsic)", "name": "en-adj" } ], "lang": "English", "lang_code": "en", "pos": "adj", "related": [ { "word": "felsite" } ], "senses": [ { "categories": [ "English terms with quotations", "en:Petrology" ], "examples": [ { "text": "Coordinate term: mafic" }, { "ref": "1954, J. C. Olson, D. R. Shawe, L. C. Pray, W. N. Sharp, Rare-Earth Mineral Deposits of the Mountain Pass District, San Bernadino County, California, U.S. Geological Survey, Professional Paper 261, page 22:", "text": "Much of the southern half of the southeastern body is a mafic syenite, slightly more felsic than the shonkinite.", "type": "quote" }, { "ref": "1983, Paul C. Bateman, “A summary of critical relations in the central part of Sierra Nevada batholith, California, U.S.A.”, in J. A. Roddick, editor, Circum-Pacific Plutonic Terranes, Geological Society of America, Memoir 159, page 241:", "text": "Within comagmatic suites, successively younger granitoids are commonly, but not invariably, more felsic, representing progressively lower temperature mineral assemblages.", "type": "quote" }, { "ref": "1992, David C. Champion, Bruce W. Chappell, “Petrogenesis of felsic I-type granites: an example from northern Queensland”, in P. E. Brown, B. W. Chappell, editor, The Second Hutton Symposium on the Origin of Granites and Related Rocks, Geological Society of America, Special Paper 272, page 115:", "text": "The Claret Creek Supersuite granites are a little more felsic (65-77% SiO₂), and are chemically distinctive, having higher Al₂O₃, CaO, Na₂O and Sr, and lower K₂O, Rb, Th and U than the granites of the Almaden Supersuite.", "type": "quote" } ], "glosses": [ "Enriched in minerals predominantly composed of the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium." ], "links": [ [ "petrology", "petrology" ] ], "raw_glosses": [ "(petrology) Enriched in minerals predominantly composed of the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium." ], "synonyms": [ { "word": "acidic" }, { "word": "sialic" }, { "word": "silicic" } ], "topics": [ "geography", "geology", "natural-sciences", "petrology" ] } ], "sounds": [ { "audio": "LL-Q1860 (eng)-Vealhurl-felsic.wav", "mp3_url": "https://upload.wikimedia.org/wikipedia/commons/transcoded/8/81/LL-Q1860_%28eng%29-Vealhurl-felsic.wav/LL-Q1860_%28eng%29-Vealhurl-felsic.wav.mp3", "ogg_url": "https://upload.wikimedia.org/wikipedia/commons/transcoded/8/81/LL-Q1860_%28eng%29-Vealhurl-felsic.wav/LL-Q1860_%28eng%29-Vealhurl-felsic.wav.ogg" } ], "word": "felsic" } { "categories": [ "English adjectives", "English blends", "English countable nouns", "English entries with incorrect language header", "English lemmas", "English nouns", "English terms suffixed with -ic", "Pages with 1 entry", "Pages with entries", "en:Rocks" ], "etymology_templates": [ { "args": { "1": "en", "2": "feldspar", "3": "silica" }, "expansion": "Blend of feldspar + silica", "name": "blend" }, { "args": { "1": "en", "2": "", "3": "ic" }, "expansion": "+ -ic", "name": "suf" } ], "etymology_text": "Blend of feldspar + silica, + -ic.", "forms": [ { "form": "felsics", "tags": [ "plural" ] } ], "head_templates": [ { "args": {}, "expansion": "felsic (plural felsics)", "name": "en-noun" } ], "lang": "English", "lang_code": "en", "pos": "noun", "senses": [ { "categories": [ "English terms with quotations" ], "examples": [ { "ref": "1953, R. C. Emmons, “Petrogeny of the Syenites and Nepheline Syenites of Central Wisconsin”, in R. C. Emmons, editor, Selected Petrogenic Relationships of Plagioclase, Geological Society of America, Memoir 52, page 80:", "text": "The central part of this nepheline syenite is very white felsics with black mafics in it. The entire area contains many nepheline-bearing dike rocks, but almost all are gray or pink or even red due to the color in the felsics.", "type": "quote" }, { "ref": "1992, T. E. Smith, chapter 1, in K. C. Condie, editor, Proterozoic Crustal Evolution, Elsevier, page 35:", "text": "There are also calcalkaline felsics that have highly enriched LREE^([light rare-earth element]) patterns with lower overall abundances.", "type": "quote" } ], "glosses": [ "A rock with such properties." ] } ], "sounds": [ { "audio": "LL-Q1860 (eng)-Vealhurl-felsic.wav", "mp3_url": "https://upload.wikimedia.org/wikipedia/commons/transcoded/8/81/LL-Q1860_%28eng%29-Vealhurl-felsic.wav/LL-Q1860_%28eng%29-Vealhurl-felsic.wav.mp3", "ogg_url": "https://upload.wikimedia.org/wikipedia/commons/transcoded/8/81/LL-Q1860_%28eng%29-Vealhurl-felsic.wav/LL-Q1860_%28eng%29-Vealhurl-felsic.wav.ogg" } ], "word": "felsic" }
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This page is a part of the kaikki.org machine-readable All languages combined dictionary. This dictionary is based on structured data extracted on 2025-02-08 from the enwiktionary dump dated 2025-02-02 using wiktextract (f90d964 and 9dbd323). The data shown on this site has been post-processed and various details (e.g., extra categories) removed, some information disambiguated, and additional data merged from other sources. See the raw data download page for the unprocessed wiktextract data.
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