In the interstices of pectolite crystals in a hyperagpaitic pegmatite.
IMA Status:
Approved IMA 1994
Locality:
In a drill core from the Oleny Stream apatite deposit in the southeastern part of the Khibina alkaline massif, Kola Peninsula, Russia. Link to MinDat.org Location Data.
Name Origin:
Name for the elements Al, Ti, and Si in the composition.
Anhedral Grains - Granular minerals without the expression of crystal shapes
Hardness:
6 - Orthoclase
Luminescence:
Non-fluorescent.
Luster:
Vitreous (Glassy)
Streak:
white
Optical Properties of Altisite
Gladstone-Dale:
CI meas= 0.025 (Excellent) - where the CI = (1-KPDmeas/KC) CI calc= 0.03 (Excellent) - where the CI = (1-KPDcalc/KC)
KPDcalc= 0.2347,KPDmeas= 0.236,KC= 0.242 Ncalc = 1.64 - 1.65
Optical Data:
Biaxial (+), a=1.601, b=1.625, g=1.654, bire=0.0530, 2V(Calc)=86, 2V(Meas)=85. Dispersion weak, r < v.
Pleochroism (x):
colorless.
Pleochroism (y):
colorless.
Pleochroism (z):
colorless.
Calculated Properties of Altisite
Electron Density:
Bulk Density (Electron Density)=2.60 gm/cc note: Specific Gravity of Altisite =2.66 gm/cc.
Fermion Index:
Fermion Index = 0.01 Boson Index = 0.99
Photoelectric:
PEAltisite = 4.79 barns/electron U=PEAltisite x relectron= 12.45 barns/cc.
Radioactivity:
GRapi = 276.29 (Gamma Ray American Petroleum Institute Units)
Concentration of Altisite per GRapi unit = 0.36 (%)
Estimated Radioactivity from Altisite - barely detectable