Krieselite (original) (raw)
A valid IMA mineral species
About KrieseliteHide
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Some of the Al is replaced by Ga, and some of the F by OH.
Specific Gravity:
4.069 (Calculated)
Crystal System:
Orthorhombic
Name:
Named in honour of Friedrich Wilhelm Kriesel (7 September 1888 - 20 September 1927), who was the chief chemist and head of the Tsumeb mine laboratory around 1920.
Ge analogue of Topaz.
The OH-dominant analogue of krieselite is known as a synthetic compound.
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:27545:1
62494a32-4673-4553-b7d3-fa388c8f39b0
IMA Classification of KrieseliteHide
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Type description reference:
Schlüter, Jochen, Geisler, Thorsten, Pohl, Dieter, Stephan, Thomas (2010) Krieselite, Al2GeO4(F,OH)2: A new mineral from the Tsumeb mine, Namibia, representing the Ge analogue of topaz. Neues Jahrbuch für Mineralogie - Abhandlungen, 187 (1) 33-40 doi:10.1127/0077-7757/2010/0160
Classification of KrieseliteHide
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9.AF.20
9 : SILICATES (Germanates)
A : Nesosilicates
F : Nesosilicates with additional anions; cations in [4], [5] and/or only [6] coordination
Mineral SymbolsHide
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As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Symbol | Source | Reference |
---|---|---|
Kes | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of KrieseliteHide
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Hardness:
VHN100=473 - 566 - Vickers
Density:
4.069 g/cm3 (Calculated)
Optical Data of KrieseliteHide
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δ = 0.000
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Comments:
The main refractive index calculated from the Gladstone-Dale relationship.
Chemistry of KrieseliteHide
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Mindat Formula:
Al2(GeO4)F2
Some of the Al is replaced by Ga, and some of the F by OH.
Crystallography of KrieseliteHide
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Crystal System:
Orthorhombic
Class (H-M):
m m m _(_2/_m_2/_m_2/m ) - Dipyramidal
Cell Parameters:
a = 9.1111 Å, b = 8.5276 Å, c = 4.8064 Å
Ratio:
a:b:c = 1.068 : 1 : 0.564
Morphology:
Observed forms: {001} and ~{110}.
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0006702 | Krieselite | Wunder B, Marler B (1997) Ge-analogues of aluminium silicates: High-pressure synthesis and properties of orthorhombic Al2GeO4(OH)2 European Journal of Mineralogy 9 1147-1158 | 1997 | 0 | 293 | ||
0018650 | Krieselite | Marler B, Wunder B (1998) Crystal structure of dialuminium dihydroxogermanate, Al2GeO4(OH)2 Zeitschrift fur Kristallographie 213 3-3 | 1998 | synthetic | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
3.811 Å | (78) |
3.315 Å | (48) |
3.016 Å | (100) |
2.464 Å | (24) |
2.417 Å | (27) |
2.247 Å | (38) |
1.398 Å | (29) |
Comments:
From type description.
Geological EnvironmentHide
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Type Occurrence of KrieseliteHide
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General Appearance of Type Material:
Hemispherical aggregates and crusts. Fibers are up to 50 × 5 μm and form wedge-shaped aggregates of fine lamellae.
Place of Conservation of Type Material:
Mineralogical Museum of the University of Hamburg, Hamburg, Germany.
Geological Setting of Type Material:
In tiny vugs of tennantite-chalcocite-galena-germanite ore.
Associated Minerals at Type Locality:
Reference:
Schlüter, J., Geisler, T., Pohl, D., Thomas, S. (2010): Krieselite, Al2GeO4(F,OH)2: A new mineral from the Tsumeb mine, Namibia, representing the Ge analogue of topaz. Neues Jahrbuch fur Mineralogie - Abhandlungen, 187, 33-40.
Synonyms of KrieseliteHide
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Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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9.AF. | Chegemite | Ca7(SiO4)3(OH)2 | Orth. m m m _(_2/_m_2/_m_2/m ) |
---|---|---|---|
9.AF. | Barwoodite | Mn2+6Nb5+(SiO4)2O3(OH)3 | Trig. 3 : _P_3 |
9.AF. | Jingwenite-(Y) | YAlV4+(SiO4)O2(OH)2 | Mon. 2/m |
9.AF.05 | Sillimanite | Al2(SiO4)O | Orth. m m m _(_2/_m_2/_m_2/m ) |
9.AF.05 | Xenolite | Al10Si8O31 | |
9.AF.10 | Andalusite | Al2(SiO4)O | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
9.AF.10 | Kanonaite | Mn3+Al(SiO4)O | Orth. m m m _(_2/_m_2/_m_2/m ) : P n n m |
9.AF.15 | Kyanite | Al2(SiO4)O | Tric. 1 : _P_1 |
9.AF.20 | Mullite | Al4+2xSi2-2xO10-x | Orth. m m m _(_2/_m_2/_m_2/m ) : P b a m |
9.AF.23 | Boromullite | Al9BSi2O19 | Orth. m _m_2 : C m _c_21 |
9.AF.25 | Yoderite | Mg(Al,Fe3+)3(SiO4)2O(OH) | Mon. 2/m : _P_21/m |
9.AF.30 | Magnesiostaurolite | Mg(Mg,Li)3(Al,Mg)18Si8O44(OH)4 | Mon. 2/m : _B_2/m |
9.AF.30 | Staurolite | Fe2+2Al9Si4O23(OH) | Mon. 2/m : _B_2/m |
9.AF.30 | Zincostaurolite | Zn2Al9Si4O23(OH) | Mon. 2/m : _B_2/m |
9.AF.35 | Topaz | Al2(SiO4)(F,OH)2 | Orth. m m m _(_2/_m_2/_m_2/m ) |
9.AF.40 | Norbergite | Mg3(SiO4)F2 | Orth. m m m _(_2/_m_2/_m_2/m ) |
9.AF.45 | Alleghanyite | Mn2+5(SiO4)2(OH)2 | Mon. 2/m : _P_21/b |
9.AF.45 | Chondrodite | Mg5(SiO4)2F2 | Mon. 2/m : _P_21/b |
9.AF.45 | Reinhardbraunsite | Ca5(SiO4)2(OH,F)2 | Mon. 2/m : _P_21/b |
9.AF.45 | Kumtyubeite | Ca5(SiO4)2F2 | Mon. 2/m : _P_21/b |
9.AF.45 | Hydroxylchondrodite | Mg5(SiO4)2(OH)2 | Mon. 2/m : _P_21/b |
9.AF.50 | Humite | Mg7(SiO4)3F2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P n m a |
9.AF.50 | Manganhumite | (Mn2+,Mg)7(SiO4)3(OH)2 | Orth. m m m _(_2/_m_2/_m_2/m ) |
9.AF.50 | Unnamed (Ca-analogue of Humite) | Ca7(SiO4)4F2 | Orth. m m m _(_2/_m_2/_m_2/m ) |
9.AF.50 | Fluorchegemite | Ca7(SiO4)3F2 | Orth. m m m _(_2/_m_2/_m_2/m ) |
9.AF.50 | Unnamed (OH-analogue of humite) | Mg7(SiO4)3(OH)2 | Orth. |
9.AF.55 | Clinohumite | Mg9(SiO4)4F2 | Mon. 2/m : _P_21/b |
9.AF.55 | Sonolite | Mn2+9(SiO4)4(OH)2 | Mon. 2/m : _P_21/b |
9.AF.55 | Hydroxylclinohumite | Mg9(SiO4)4(OH)2 | Mon. 2/m : _P_21/b |
9.AF.60 | Leucophoenicite | Mn2+7(SiO4)3(OH)2 | Mon. 2/m : _P_21/b |
9.AF.65 | Ribbeite | Mn2+5(SiO4)2(OH)2 | Orth. m m m _(_2/_m_2/_m_2/m ) |
9.AF.70 | Jerrygibbsite | Mn2+9(SiO4)4(OH)2 | Orth. m m m _(_2/_m_2/_m_2/m ) : P b c n |
9.AF.75 | Franciscanite | Mn2+6(V5+,◻)2(SiO4)2(O,OH)6 | Trig. 3 : _P_3 |
9.AF.75 | Örebroite | Mn2+3(Sb5+,Fe3+)(SiO4)(O,OH)3 | Trig. 3 : _P_3 |
9.AF.75 | Welinite | Mn2+6(W6+,Mg)2(SiO4)2(O,OH)6 | Trig. 3 : _P_3 |
9.AF.75 | Scorticoite | Mn6(Sb,◻)Σ2(SiO4)2O3(OH)3 | Trig. 3 : _P_3 |
9.AF.80 | Ellenbergerite | Mg6(Mg,Ti,Zr,◻)2(Al,Mg)6Si8O28(OH)10 | Hex. 6 : _P_63 |
9.AF.85 | Chloritoid | Fe2+Al2O(SiO4)(OH)2 | Mon. 2/m : _B_2/b |
9.AF.85 | Magnesiochloritoid | MgAl2O(SiO4)(OH)2 | Mon. 2/m : _B_2/b |
9.AF.85 | Ottrélite | Mn2+Al2O(SiO4)(OH)2 | Mon. |
9.AF.90 | Poldervaartite | CaCa[SiO3(OH)](OH) | Orth. m m m _(_2/_m_2/_m_2/m ) : P b c a |
9.AF.90 | Olmiite | CaMn2+[SiO3(OH)](OH) | Orth. m m m _(_2/_m_2/_m_2/m ) : P b c a |
9.AF.95 | Pilawite-(Y) | Ca2Y2Al4(SiO4)4O2(OH)2 | Mon. 2/m : _P_21/b |
Other InformationHide
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Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Internet Links for KrieseliteHide
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References for KrieseliteHide
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Reference List:
Schlüter, Jochen, Geisler, Thorsten, Pohl, Dieter, Stephan, Thomas (2010) Krieselite, Al2GeO4(F,OH)2: A new mineral from the Tsumeb mine, Namibia, representing the Ge analogue of topaz. Neues Jahrbuch für Mineralogie - Abhandlungen, 187 (1) 33-40 doi:10.1127/0077-7757/2010/0160
Localities for KrieseliteHide
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This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.
Locality ListHide
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- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).
All localities listed without proper references should be considered as questionable.
Namibia (TL) | |
---|---|
Oshikoto Region Tsumeb ⓘ Tsumeb Mine (Ongopolo Mine) (TL) | Schlüter et al. (2010) |