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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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mineral origin references ferropericlase high pressure calcium silicate casio3 found diamond inclusions second abundant inclusion diamonds deep earth occurrence also
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Breyite | Category | Minerals | 1.00 | infobox |
| Breyite | Cleavage | not observed | 1.00 | infobox |
| Breyite | Colour | colorless | 1.00 | infobox |
| Breyite | Crystal system | Triclinic | 1.00 | infobox |
| Breyite | Density | 3.072 g/cm3 | 1.00 | infobox |
| Breyite | Formula | Ca3.01(2)Si2.98(2)O9 | 1.00 | infobox |
| Breyite | IMA symbol | Byi | 1.00 | infobox |
| Breyite | Luster | vitreous | 1.00 | infobox |
| Breyite | Space group | P1 | 1.00 | infobox |
| Breyite | Ultraviolet fluorescence | non-fluorescent | 1.00 | infobox |
| Breyite | Unit cell | a0 = 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)° | 1.00 | infobox |
| Breyite | is a | high pressure calcium silicate mineral | 0.90 | text |
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