Images
  
  Formula: YCa2Zr2Al3O12 
  
  Oxide, garnet supergroup, yttrium- 
  and zirconium- bearing mineral
  
  Crystal System: Isometric
  
  Specific gravity: 4.48 calculated
  
  Hardness: 7 to 7½
  
  Colour: Pale yellowish tinge
  
  Environments
  
  Sedimentary environments
  
Metamorphic environments
  Priscillagrewite-(Y) is a new mineral, approved in 2020. It is an unusual member of the 
  bitikleite group within the garnet 
  supergroup, related to rubinite and 
  eringaite, that are garnets thought 
  to be some of the first solids to crystallise in the solar nebula 
  R&M 97.5.461-463).
  
  Localities
  
  At the type locality, the Daba marble quarry, Daba, Daba-Siwaqa complex, Transjordan Plateau, Amman Governorate, 
  Jordan, the formation consists of apatite layered 
  marble from protoliths of bituminous 
  marls, and limestone 
  intercalated with phosphorite. 
  
  Priscillagrewite-(Y) occurs as diomorphic (having two different forms), isometric crystals up to 15 μm in size. 
  
  It is suggested that the source material for priscillagrewite-(Y) is not from rare-earth-element containing 
  phosphatic 
  minerals such as fluorapatite, but likely from detrital 
  zircon as the source of both the zirconium and the 
  yttrium 
  (AM 107.318).
  
  Priscillagrewite-(Y) occurs as tiny transparent, undistorted crystals with a pale yellow tint and vitreous 
  lustre. The matrix is a green fluorapatite and 
  spurrite layer coloured by vanadium 
  that also includes irregular distributions of baghdadite, 
  cuprite, ellinaite, 
  fluormayenite, hematite, 
  lakargiite, mcconnellite, 
  perovskite (both yttrium-bearing 
  and yttrium-free), sphalerite, 
  tululite, vapnikite and 
  zincite, as well as members of the 
  andradite-grossular series, 
  members of the 
  brownmillerite-srebrodolskite 
  series, members of the 
  lime-monteponite series and members 
  of the 
  magnesiochromite-zincochromite 
  series. 
  
  The rock layer in which priscillagrewite-(Y) was discovered was converted to 
  marble by pyrometamorphism that may have reached 1,000°C. The 
  pyrometamorphism appears to have resulted from the burning of plentiful hydrocarbons in the preexisting 
  limestone  
  R&M 97.5.461-463).
  
 
  Back to Minerals