General Bushmakinite Information Chemical Formula: |
Pb2Al(PO4)(VO4)(OH) |
Composition: |
Molecular Weight = 667.89 gm |
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Aluminum 3.11 % Al 5.88 % Al2O3 |
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Vanadium 5.64 % V 10.08 % V2O5 |
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Zinc 0.10 % Zn 0.12 % ZnO |
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Chromium 1.09 % Cr 2.10 % CrO3 |
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Copper 2.00 % Cu 2.50 % CuO |
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Phosphorus 4.64 % P 10.63 % P2O5 |
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Hydrogen 0.15 % H 1.38 % H2O |
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Lead 62.67 % Pb 67.51 % PbO |
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Sulfur 0.05 % S 0.12 % SO3 |
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Oxygen 20.55 % O |
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______ ______ |
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100.00 % 100.30 % = TOTAL OXIDE |
Empirical Formula: |
Pb2.02Al0.77Cu0.21Zn0.01(PO4)(VO4)0.74(CrO4)0.14SO40.01(OH)1.02 |
Environment: |
Oxidation of galena and tetrahedrite in a quartz vein. (brackebuschite group; structure) |
IMA Status: |
Approved IMA 2002, Dana # Added |
Locality: |
Berezovskoye gold deposit, middle Ural Mountains, Russia. Link to MinDat.org Location Data. |
Name Origin: |
Named for Anatolly F. Bushmakin (1947-1999), in recognition of his work on the Berezovskoye deposit. |
Synonym: |
IMA2001-031 |
| | Bushmakinite Image
Images:
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Bushmakinite Crystallography Axial Ratios: |
a:b:c =1.3302:1:1.4946 |
Cell Dimensions: |
a = 7.734, b = 5.814, c = 8.69, Z = 2; beta = 112.1° V = 362.04 Den(Calc)= 6.13 |
Crystal System: |
Monoclinic - PrismaticH-M Symbol (2/m) Space Group: P 21/m |
X Ray Diffraction: |
By Intensity(I/Io): 3.21(1)(211), 4.68(0.8)(011), 2.91(0.7)(212,020,103),2.71(0.7)(021,122), 2.05(0.5)(123,114), 3.57(0.5)(111,200), 2.27(0.4),
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Crystal Structure:
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Mouse
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| Physical Properties of Bushmakinite Cleavage: |
{001} Perfect, {hk0} Distinct, {hk0} Distinct |
Color: |
Bright yellow. |
Diaphaneity: |
Translucent |
Fracture: |
Brittle - Generally displayed by glasses and most non-metallic minerals. |
Habit: |
Granular - Generally occurs as anhedral to subhedral crystals in matrix. |
Habit: |
Lamellar - Thin laminae producing a lamellar structure. |
Hardness: |
3-3.5 - Calcite-Copper Penny |
Luster: |
Vitreous (Glassy) |
Streak: |
yellowish |
| Optical Properties of Bushmakinite Gladstone-Dale: |
CI calc= 0.026 (Excellent) - where the CI = (1-KPDcalc/KC) |
KPDcalc= 0.1675,KC= 0.172 Ncalc = 2.05 Optical Data: |
Biaxial (-), a=1.99, b=2.03, g=2.06, bire=0.0700, 2V(Calc)=80, 2V(Meas)=large. Dispersion appreciable, r < v. |
| Calculated Properties of Bushmakinite Electron Density: |
Bulk Density (Electron Density)=5.27 gm/cc |
note: Specific Gravity of Bushmakinite =6.13 gm/cc. Fermion Index: |
Fermion Index = 0.13 |
Boson Index = 0.87 Photoelectric: |
PEBushmakinite =1,121.29 barns/electron |
U=PEBushmakinite x rElectron Density=5,912.17 barns/cc. Radioactivity: |
GRapi = 0 (Gamma Ray American Petroleum Institute Units) |
Bushmakinite is Not Radioactive | Bushmakinite Classification Dana Class: |
40.02.08.05 (40)Hydrated Phosphates, etc |
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(40.02)where A++ (B++)2 (XO4) · x(H2O) |
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(40.02.08)Brackebushite Group |
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Strunz Class: |
08.BG.05 08 - PHOSPHATES, ARSENATES, VANADATES |
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08.B - Phosphates, etc. with Additional Anions, without H2O |
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08.BG -With medium-sized and large cations, (OH, etc.):RO4 = 0.5:1 |
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| Other Bushmakinite Information References: |
NAME( AmMin, Vol 88, p 475) PHYS. PROP.(AmMin, Vol 88, p 475) OPTIC PROP.(AmMin, Vol 88, p 475) |
See Also: |
Links to other databases for Bushmakinite : |
1 - Am. Min. Crystal Structure Database 2 - Athena 3 - GeoScienceWorld 4 - Google Images 5 - Google Scholar 6 - MinDAT 7 - Mineralienatlas (Deutsch) 8 - Online Mineral Museum 9 - QUT Mineral Atlas 10 - Ruff.Info Search for Bushmakinite using: Visit our Advertisers for Bushmakinite : A Bijoux Google Search for BushmakiniteAdam's Minerals Google Search for Bushmakinite Cape Minerals Google Search for Bushmakinite Dakota Matrix Minerals Google Search for Bushmakinite Excalibur Mineral Corp. Google Search for Bushmakinite Exceptional Minerals Google Search for Bushmakinite John Betts Fine Minerals Search for Bushmakinite McDougall Minerals Google Search for Bushmakinite Mineral News Website Link Rock and Mineral Shows Google Search for Bushmakinite Weinrich Minerals, Inc. Google Search for Bushmakinite Ask about Bushmakinite here : Print or Cut-and-Paste your Bushmakinite Specimen Label here :
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