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Breyite

Breyite is a high pressure calcium silicate mineral (CaSiO3) found in diamond inclusions. It is the second most abundant inclusion after ferropericlase, for diamonds with a deep Earth origin. Its occurrence can also indicate the host diamond's super-deep origin. This mineral is named after German mineralogist, petrologist and geochemist Gerhard P. Brey.

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1 related topics

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Category
Minerals
Cleavage
not observed
Colour
colorless
Crystal system
Triclinic
Density
3.072 g/cm3
Formula
Ca3.01(2)Si2.98(2)O9

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Breyite

Nodes3
Edges2
Triples12
Avg. degree1.33
Density0.666667
Components1

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Breyite

Top relations

Category · 1
Breyite → Minerals
Cleavage · 1
Breyite → not observed
Colour · 1
Breyite → colorless
Crystal system · 1
Breyite → Triclinic
Density · 1
Breyite → 3.072 g/cm3
Formula · 1
Breyite → Ca3.01(2)Si2.98(2)O9
IMA symbol · 1
Breyite → Byi
Luster · 1
Breyite → vitreous
Space group · 1
Breyite → P1
Ultraviolet fluorescence · 1
Breyite → non-fluorescent

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Important terminology

mineral origin references ferropericlase high pressure calcium silicate casio3 found diamond inclusions second abundant inclusion diamonds deep earth occurrence also

Entity relationships Subject–Predicate–Object triples

SubjectPredicateObjectConfidenceSrc
BreyiteCategoryMinerals1.00infobox
BreyiteCleavagenot observed1.00infobox
BreyiteColourcolorless1.00infobox
BreyiteCrystal systemTriclinic1.00infobox
BreyiteDensity3.072 g/cm31.00infobox
BreyiteFormulaCa3.01(2)Si2.98(2)O91.00infobox
BreyiteIMA symbolByi1.00infobox
BreyiteLustervitreous1.00infobox
BreyiteSpace groupP11.00infobox
BreyiteUltraviolet fluorescencenon-fluorescent1.00infobox
BreyiteUnit cella0 = 6.6970(4) Å, b0= 9.2986(7) Å, c0 = 6.6501(4) Å, α = 83.458(6)°, β = 76.226(6)°, γ = 69.581(7)°1.00infobox
Breyiteis ahigh pressure calcium silicate mineral0.90text

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