[Thumbnails] [Miniatures] [Cabinets] [About Us] [FAQ] Welcome To Mason's Minerals Your Source for Beautiful Minerals and Crystals We offer a no-questioned-asked Satisfaction Guarantee General Phosphoinnelite InformationBa4Na3Ti3Si4O14(PO4,SO4)2(O,F)3 |
Molecular Weight = 1,301.51 gm |
|
Potassium 0.03 % K 0.04 % K2O |
|
Barium 37.88 % Ba 42.29 % BaO |
|
Sodium 4.57 % Na 6.17 % Na2O |
|
Strontium 0.88 % Sr 1.03 % SrO |
|
Calcium 0.12 % Ca 0.17 % CaO |
|
Magnesium 0.39 % Mg 0.65 % MgO |
|
Titanium 10.30 % Ti 17.18 % TiO2 |
|
Niobium 0.50 % Nb 0.71 % Nb2O5 |
|
Aluminum 0.15 % Al 0.27 % Al2O3 |
|
Iron 1.12 % Fe 1.60 % Fe2O3 |
|
Silicon 8.48 % Si 18.14 % SiO2 |
|
Phosphorus 2.64 % P 6.05 % P2O5 |
|
Sulfur 2.14 % S 5.35 % SO3 |
|
Oxygen 30.65 % O |
|
Fluorine 0.15 % F 0.15 % F |
|
- %
F -0.06 % -O=F2 |
|
______ ______ |
|
100.00 % 99.75 % = TOTAL OXIDE |
Ba3.59Sr0.13K0.01Na2.59Mg0.21Ca0.04Ti2.8Fe3+0.26Nb0.07Si3.93Al0.07O14P1.11S0.87O7.96
O2.97F0.1 |
Found in peralkaline pegmatite vein crosscutting calcite carbonatite at a phlogopite deposit. Bafertisite series |
Approved IMA 2005 (Dana # Added) |
Mica Mine, Kovdor alkaline-ultramafic complex, Kola Peninsula, Russia Link to MinDat.org Location Data. |
Named as the P analog of innelite. |
IMA2005-022 |
| | Phosphoinnelite Image
|
|
Phosphoinnelite Crystallographya:b:c =0.7577:1:2.0788 |
a = 5.38, b = 7.1, c = 14.76, Z = 1; alpha = 99°, beta = 94.94°, gamma = 90.14° V = 554.79 Den(Calc)= 3.90 |
TriclinicSpace Group: P1 or P1 |
By Intensity(I/Io): 14.5(1), 2.683(0.9), 2.133(0.8),2.059(0.4), 2.81(0.4), 3.455(0.4), 2.921(0.35), 3.382(0.35), |
| Physical Properties of Phosphoinnelite3.82 |
Transparent |
Brittle - Generally displayed by glasses and most non-metallic minerals. |
Lath - Shaped like a small, thin plaster lath, tabular (rectangular) in shape. |
Rosette - Bundled tabular aggregates resembling rose flower petals. |
Wheat Sheaf - Bundle shaped aggregates resembling wheat sheafs after hand reaping wheat. |
4.5-5 - Near Apatite |
Vitreous - Greasy |
pale yellow |
| Optical Properties of PhosphoinneliteCI meas= 0.035 (Excellent) - where the CI = (1-KPDmeas/KC) |
CI calc= 0.055 (Good) - where the CI = (1-KPDcalc/KC) KPDcalc= 0.1914,KPDmeas= 0.1954,KC= 0.2025 Ncalc = 1.77 - 1.79 Biaxial (+), a=1.73, b=1.745, g=1.764, bire=0.0340 |
| Calculated Properties of PhosphoinneliteBulk Density (Electron Density)=3.50 gm/cc |
note: Specific Gravity of Phosphoinnelite =3.82 gm/cc. Fermion Index = 0.08 |
Boson Index = 0.92 PEPhosphoinnelite = 170.42 barns/electron |
U=PEPhosphoinnelite x relectron= 596.30 barns/cc. |
GRapi = 0.39 (Gamma Ray American Petroleum Institute Units)
Estimated Radioactivity from Phosphoinnelite | Phosphoinnelite Classification58.02.06.03 (58)Sorosilicate Insular, Mixed, Single, and Larger Tetrahedral Groups |
|
(58.02)with cations in [6] and higher coordination; single and double groups (n=1,2) |
|
(58.02.06)Yoshimuraite and related species |
|
|
|
09.BE.40 09 - SILICATES (Germanates) |
|
09.B - Sorosilicates |
|
09.BE -Si2O7 groups with additional anions; |
|
|
| Other Phosphoinnelite InformationNAME( Geology of Ore Deposits, v49:530) PHYS. PROP.( Geology of Ore Deposits, v49:530) OPTIC PROP.( Geology of Ore Deposits, v49:530) |
Links to other databases for Phosphoinnelite : |
1 - Am. Min. Crystal Structure Database 2 - Athena 3 - Google Images 4 - Google Scholar 5 - MinDAT 6 - MinMax(Deutsch) 7 - MinMax(English) 8 - Mineralienatlas (Deutsch) 9 - QUT Mineral Atlas 10 - Ruff.Info Search for Phosphoinnelite using: Visit our Advertisers for Phosphoinnelite : AA Mineral SpecimensB & L Fine Minerals Crystalarium.com Dan Weinrich Fine Minerals Dan Weinrich Auctions Dakota Matrix Diamond Dan Publications e-Rocks Auctions Excalibur Minerals Exceptional Minerals Heliodor John Betts Fine Minerals Mason's Minerals Mineral News Mineral of the Month Club Wrights Rock Shop Translate Phosphoinnelite Mineral Data : Ask about Phosphoinnelite here : Print or Cut-and-Paste your Phosphoinnelite Specimen Label here :
| |
|
| | |||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||