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Breyite

Summary

Breyite is a high pressure calcium silicate mineral (CaSiO3) found in diamond inclusions.[3][4] It is the second most abundant inclusion after ferropericlase, for diamonds with a deep Earth origin.[5][4] 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.

Breyite
General
CategoryMineral
Formula
(repeating unit)		Ca3.01(2)Si2.98(2)O9
IMA symbolByi[1]
Crystal systemTriclinic
Space groupP1
Unit 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)°
Identification
Colourcolorless
Cleavagenot observed
Lustervitreous
Density3.072 g/cm3
Ultraviolet fluorescencenon-fluorescent
References[2]
CaSiO3 phase diagram showing Breyite is stable around 3-9 GPa[6]

References edit

  1. ^ "Breyite". www.mindat.org. Retrieved 2022-01-15.
  2. ^ Brenker, Frank E.; Nestola, Fabrizio; Brenker, Lion; Peruzzo, Luca; Harris, Jeffrey W. (1 January 2021). "Origin, properties, and structure of breyite: The second most abundant mineral inclusion in super-deep diamonds". American Mineralogist. 106 (1): 38–43. Bibcode:2021AmMin.106...38B. doi:10.2138/am-2020-7513. S2CID 231543488.
  3. ^ Alderton, David; Elias, Scott (2020). Encyclopedia of Geology. Elsevier Science. p. 467. ISBN 9780081029091.
  4. ^ a b Brenker, Frank E.; Nestola, Fabrizio; Brenker, Lion; Peruzzo, Luca; Harris, Jeffrey W. (2021-01-01). "Origin, properties, and structure of breyite: The second most abundant mineral inclusion in super-deep diamonds". American Mineralogist. 106 (1): 38–43. Bibcode:2021AmMin.106...38B. doi:10.2138/am-2020-7513. ISSN 1945-3027. S2CID 231543488.
  5. ^ "Breyite". www.mindat.org. Retrieved 2022-01-15.
  6. ^ Milani, Sula; Comboni, Davide; Lotti, Paolo; Fumagalli, Patrizia; Ziberna, Luca; Maurice, Juliette; Hanfland, Michael; Merlini, Marco (2021-06-19). "Crystal Structure Evolution of CaSiO3 Polymorphs at Earth's Mantle Pressures". Minerals. 11 (6): 652. Bibcode:2021Mine...11..652M. doi:10.3390/min11060652. hdl:11368/2993918. ISSN 2075-163X.