About: Plagioclase

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About: Plagioclase Sponge Permalink

An Entity of Type : dbkwik:resource/mN1SPtSK6DqXcZx381QGPQ==, within Data Space : 134.155.108.49:8890 associated with source dataset(s)

Plagioclase refers to a group of feldspar minerals that exist in solid solution between Albite (NaAlSi3O8) and Anorthite (CaAl2Si2O8) endmembers. The range of minerals include Albite, Oligoclase, Andesine, Labradorite, Bytownite, and Anorthite. Each mineral represents a specific composition between albite and anorthite. It is a major component of the Earth's crust.

Attributes	Values
rdf:type	Rock
rdfs:label	Plagioclase
rdfs:comment	Plagioclase refers to a group of feldspar minerals that exist in solid solution between Albite (NaAlSi3O8) and Anorthite (CaAl2Si2O8) endmembers. The range of minerals include Albite, Oligoclase, Andesine, Labradorite, Bytownite, and Anorthite. Each mineral represents a specific composition between albite and anorthite. It is a major component of the Earth's crust.
sameAs	dbr:Plagioclase
dcterms:subject	Minerals Feldspar
cleave	Perfect
Name	Plagioclase
Type	Feldspar
dbkwik:geology/pro...iPageUsesTemplate	dbkwik:resource/XT6LQEmK8k32kN-BS-1rAA==
SG	2(xsd:double)
streak	white
Hard	6(xsd:integer)
RM	Mineral
Pro	Puh-la-gee-oh-klaise
lust	vitreous
chemcomp	NaAlSi3O8 – CaAl2Si2O8
abstract	Plagioclase refers to a group of feldspar minerals that exist in solid solution between Albite (NaAlSi3O8) and Anorthite (CaAl2Si2O8) endmembers. The range of minerals include Albite, Oligoclase, Andesine, Labradorite, Bytownite, and Anorthite. Each mineral represents a specific composition between albite and anorthite. It is a major component of the Earth's crust.
is essential mineral(s) of	Granite

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