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Statements

Subject Item
dbr:Hypersolvus
rdfs:label
Hypersolvus
rdfs:comment
In hypersolvus granites, as used by Tuttle and Bowen in 1958, crystallization at relatively low water pressures results in the formation of a single feldspar as opposed to subsolvus granites in which two distinct types of feldspar are present.
dcterms:subject
dbc:Igneous_petrology
dbo:wikiPageID
9213038
dbo:wikiPageRevisionID
1038564217
dbo:wikiPageWikiLink
dbr:Granites dbr:Feldspar dbr:Ternary_form dbr:Subsolvus dbr:Perthite dbr:Exsolution dbc:Igneous_petrology
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freebase:m.0280hf8 n9:4n3UQ wikidata:Q5958578
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dbo:abstract
In hypersolvus granites, as used by Tuttle and Bowen in 1958, crystallization at relatively low water pressures results in the formation of a single feldspar as opposed to subsolvus granites in which two distinct types of feldspar are present. The distinctive character of feldspar in hypersolvus granite is to present exsolution textures. That is because the high temperature feldspar was ternary (i.e. contained comparable parts of the Ca, Na, K components) and was later dissociated during the cooling phase into K-rich parts and Na-Ca-rich parts, within the initial crystal. The resulting texture is referred to as perthitic.
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wikipedia-en:Hypersolvus?oldid=1038564217&ns=0
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1085
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wikipedia-en:Hypersolvus