See felsic in All languages combined, or Wiktionary
{
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"forms": [
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"form": "more felsic",
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"pos": "adj",
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"word": "mafic"
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"word": "felsification"
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"word": "nonfelsic"
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"examples": [
{
"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, U.S. Department of the Interior, page 22:",
"text": "Much of the southern half of the southeastern body is a mafic syenite, slightly more felsic than the shonkinite.",
"type": "quote"
},
{
"text": "1983, Paul C. Bateman, A summary of critical relations in the central part of Sierra Nevada batholith, California, U.S.A., J. A. Roddick (editor), Circum-Pacific Plutonic Terranes, Geological Society of America Memoir 159, page 241,\nWithin comagmatic suites, successively younger granitoids are commonly, but not invariably, more felsic, representing progressively lower temperature mineral assemblages."
},
{
"text": "1992, David C. Champion, Bruce W. Chappell, Petrogenesis of felsic I-type granites: an example from northern Queensland, P. E. Brown, B. W. Chappell (editors), The Second Hutton Symposium on the Origin of Granites and Related Rocks, Proceedings, Geological Society of America Special Paper 272, [Originally published in Transactions of the Royal Society of Edinburgh: Earth Sciences, Volume 83], page 115,\nThe 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."
}
],
"glosses": [
"Enriched in minerals predominantly composed of the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium."
],
"id": "en-felsic-en-adj-tdFxHYTn",
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[
"petrology",
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"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": "silicic"
},
{
"word": "sialic"
}
],
"topics": [
"geography",
"geology",
"natural-sciences",
"petrology"
]
}
],
"word": "felsic"
}
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"etymology_text": "Blend of feldspar + silica, + -ic.",
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{
"form": "felsics",
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"text": "1953, R. C. Emmons, Chapter 6: Petrogeny of the Syenites and Nepheline Syenites of Central Wisconsin, R. C. Emmons (editor), Selected Petrogenic Relationships of Plagioclase, Geological Society of America Memoir 52, page 80,\nThe 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."
},
{
"ref": "1992, T. E. Smith, “Chapter 1: Volcanic Rocks of Early Proterozoic Greenstone Belts”, 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"
}
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"A rock with such properties."
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"id": "en-felsic-en-noun-smHsDz7V"
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},
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"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, U.S. Department of the Interior, page 22:",
"text": "Much of the southern half of the southeastern body is a mafic syenite, slightly more felsic than the shonkinite.",
"type": "quote"
},
{
"text": "1983, Paul C. Bateman, A summary of critical relations in the central part of Sierra Nevada batholith, California, U.S.A., J. A. Roddick (editor), Circum-Pacific Plutonic Terranes, Geological Society of America Memoir 159, page 241,\nWithin comagmatic suites, successively younger granitoids are commonly, but not invariably, more felsic, representing progressively lower temperature mineral assemblages."
},
{
"text": "1992, David C. Champion, Bruce W. Chappell, Petrogenesis of felsic I-type granites: an example from northern Queensland, P. E. Brown, B. W. Chappell (editors), The Second Hutton Symposium on the Origin of Granites and Related Rocks, Proceedings, Geological Society of America Special Paper 272, [Originally published in Transactions of the Royal Society of Edinburgh: Earth Sciences, Volume 83], page 115,\nThe 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."
}
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"Enriched in minerals predominantly composed of the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium."
],
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"petrology",
"petrology"
]
],
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"(petrology) Enriched in minerals predominantly composed of the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium."
],
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"geography",
"geology",
"natural-sciences",
"petrology"
]
}
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"word": "acidic"
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{
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],
"word": "felsic"
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{
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{
"text": "1953, R. C. Emmons, Chapter 6: Petrogeny of the Syenites and Nepheline Syenites of Central Wisconsin, R. C. Emmons (editor), Selected Petrogenic Relationships of Plagioclase, Geological Society of America Memoir 52, page 80,\nThe 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."
},
{
"ref": "1992, T. E. Smith, “Chapter 1: Volcanic Rocks of Early Proterozoic Greenstone Belts”, 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."
]
}
],
"word": "felsic"
}
Download raw JSONL data for felsic meaning in English (4.6kB)
This page is a part of the kaikki.org machine-readable English dictionary. This dictionary is based on structured data extracted on 2025-02-03 from the enwiktionary dump dated 2025-01-20 using wiktextract (05fdf6b 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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