Trögerite
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About Trögerite
Formula:
(H3O)(UO2)(AsO4) · 3H2O
There is a considerable confusion in the literature in distinguishing amongst two independent species, (meta)hydroniumuranospinite (structure based upon autunite topology), and trögerite (structure based upon different topology, as indicated by U:As ratio equal 3:2, c.f. original description by Weissbach 1873). Locock et al. (2004) introduced a misleading assignment of trögerite to the autunite group, with the composition (H3O)2[(UO2)2(AsO4)2](H2O)6. Chernorukov et al. (2011) synthesized compound of the composition (UO2)3(AsO4)2(H2O)12, which they equalized with trögerite. Structural investigations of Locock and Burns (2002) on synthetic (UO2)3(PO4)2(H2O)4, which is based on uranophane topology, suggests, that trögerite may be based on similar topology, having a framework structure with uranium located both on sheets as well as in interlayer, similarly as e.g. phosphuranylite (Demartin et al. 1991). The chemical composition of trögerite given in original description by Weissbach (1873) suggests that these two substances are not same mineral. Recently electron microanalysis of the type material of trögerite documented neither presence of trögerite on it nor the presence of (H3O)2[(UO2)2(AsO4)2](H2O)6. All analyzed crystals belong to nováčekite (Plášil et al. in prep.)
Colour:
Lemon-yellow, to deep yellow
Lustre:
Sub-Vitreous, Waxy, Pearly
Hardness:
2 - 3
Specific Gravity:
3.3 - 3.55
Crystal System:
Tetragonal
Member of:
Name:
Named by A. Weisbach in 1871 for "R. Troeger", possibly for Richard Otto Troeger [1838-1917], mining administrator at Schneeberg, Saxony, Germany. (The translation of 'Bergverwalter' (= mining administrator) may indicate a lesser position such as mine captain, mine superintendent, or shift boss.)
Possibly the arsenate analogue of 'UM1963-03-PO:HU'. Compare 'Unnamed (Hydronium-uranyl arsenate)', a chemically similar phase.
A secondary mineral usually found as crusts or aggregates of microscopic crystals. Often found growing in parallel with zeunerite.
A secondary mineral usually found as crusts or aggregates of microscopic crystals. Often found growing in parallel with zeunerite.
Classification of Trögerite
Approved, 'Grandfathered' (first described prior to 1959)
7/E.01-10
8.EB.15
8 : PHOSPHATES, ARSENATES, VANADATES
E : Uranyl phosphates and arsenates
B : UO2:RO4 = 1:1
8 : PHOSPHATES, ARSENATES, VANADATES
E : Uranyl phosphates and arsenates
B : UO2:RO4 = 1:1
Dana 7th ed.:
40.2.20.1
40.2a.20.1
40 : HYDRATED NORMAL PHOSPHATES,ARSENATES AND VANADATES
2a : AB2(XO4)2·xH2O, containing (UO2)2+
40 : HYDRATED NORMAL PHOSPHATES,ARSENATES AND VANADATES
2a : AB2(XO4)2·xH2O, containing (UO2)2+
20.7.1
20 : Arsenates (also arsenates with phosphate, but without other anions)
7 : Arsenates of U
20 : Arsenates (also arsenates with phosphate, but without other anions)
7 : Arsenates of U
Physical Properties of Trögerite
Sub-Vitreous, Waxy, Pearly
Transparency:
Transparent, Translucent
Comment:
pearly on the {001} cleavage.
Colour:
Lemon-yellow, to deep yellow
Streak:
White to pale yellow
Hardness:
2 - 3 on Mohs scale
Hardness Data:
Measured
Tenacity:
Brittle
Cleavage:
Perfect
Perfect on {001}, on {100} good; on {011} poor or in traces.
Perfect on {001}, on {100} good; on {011} poor or in traces.
Fracture:
Micaceous
Density:
3.3 - 3.55 g/cm3 (Measured) 4.80 g/cm3 (Calculated)
Comment:
D has been calculated up to 5.13 (HB v4). Discrepancy is unexplained.
Optical Data of Trögerite
Type:
Uniaxial (-)
RI values:
nα = 1.585 nβ = 1.630 nγ = 1.630 nω = 1.580 nε = 1.620 - 1.624
Birefringence:
0.045
Max Birefringence:
δ = 0.040

Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
and does not take into account mineral colouration.
Surface Relief:
Moderate
Dispersion:
r > v
Optical Extinction:
Anomalously biaxial, X=c, Z ^ a = 13°, 2° = very small nearly zero
Pleochroism:
Visible
Comments:
O = Y = Z = Lemon-yellow
E = X = Nearly colourless
E = X = Nearly colourless
Comments:
May be biaxial -, probably anomalous, zoned due to differences in H2O content.
Chemical Properties of Trögerite
Formula:
(H3O)(UO2)(AsO4) · 3H2O
There is a considerable confusion in the literature in distinguishing amongst two independent species, (meta)hydroniumuranospinite (structure based upon autunite topology), and trögerite (structure based upon different topology, as indicated by U:As ratio equal 3:2, c.f. original description by Weissbach 1873). Locock et al. (2004) introduced a misleading assignment of trögerite to the autunite group, with the composition (H3O)2[(UO2)2(AsO4)2](H2O)6. Chernorukov et al. (2011) synthesized compound of the composition (UO2)3(AsO4)2(H2O)12, which they equalized with trögerite. Structural investigations of Locock and Burns (2002) on synthetic (UO2)3(PO4)2(H2O)4, which is based on uranophane topology, suggests, that trögerite may be based on similar topology, having a framework structure with uranium located both on sheets as well as in interlayer, similarly as e.g. phosphuranylite (Demartin et al. 1991). The chemical composition of trögerite given in original description by Weissbach (1873) suggests that these two substances are not same mineral. Recently electron microanalysis of the type material of trögerite documented neither presence of trögerite on it nor the presence of (H3O)2[(UO2)2(AsO4)2](H2O)6. All analyzed crystals belong to nováčekite (Plášil et al. in prep.)
There is a considerable confusion in the literature in distinguishing amongst two independent species, (meta)hydroniumuranospinite (structure based upon autunite topology), and trögerite (structure based upon different topology, as indicated by U:As ratio equal 3:2, c.f. original description by Weissbach 1873). Locock et al. (2004) introduced a misleading assignment of trögerite to the autunite group, with the composition (H3O)2[(UO2)2(AsO4)2](H2O)6. Chernorukov et al. (2011) synthesized compound of the composition (UO2)3(AsO4)2(H2O)12, which they equalized with trögerite. Structural investigations of Locock and Burns (2002) on synthetic (UO2)3(PO4)2(H2O)4, which is based on uranophane topology, suggests, that trögerite may be based on similar topology, having a framework structure with uranium located both on sheets as well as in interlayer, similarly as e.g. phosphuranylite (Demartin et al. 1991). The chemical composition of trögerite given in original description by Weissbach (1873) suggests that these two substances are not same mineral. Recently electron microanalysis of the type material of trögerite documented neither presence of trögerite on it nor the presence of (H3O)2[(UO2)2(AsO4)2](H2O)6. All analyzed crystals belong to nováčekite (Plášil et al. in prep.)
Elements listed:
Crystallography of Trögerite
Crystal System:
Tetragonal
Class (H-M):
4/mmm (4/m 2/m 2/m) - Ditetragonal Dipyramidal
Space Group:
P4/nmm
Setting:
P4/nmm
Cell Parameters:
a = 7.16 Å, c = 8.80 Å
Ratio:
a:c = 1 : 1.229
Unit Cell V:
451.14 ų (Calculated from Unit Cell)
Z:
1
Morphology:
Elongated thin tabular {001}, often composite and uneven; nonpinacoidal forms asymmetrically developed, implying a Monoclinic symmetry; other faces small and striated horizontally. Found as crusts or aggregates of microscopic crystals, often found growing in parallel with zeunerite.
Twinning:
None reported.
Epitaxial Relationships of Trögerite
Epitaxial Minerals:
Zeunerite | Cu(UO2)2(AsO4)2 · 12H2O |
Epitaxy Comments:
Zeunerite crystals commonly occur overgrowing Trögerite in parallel position.
X-Ray Powder Diffraction
Powder Diffraction Data:
d-spacing | Intensity |
---|---|
8.59 Å | (100) |
5.50 Å | (70) |
4.35 Å | (70) |
3.79 Å | (90) |
3.30 Å | (80) |
2.70 Å | (70) |
2.19 Å | (70) |
2.01 Å | (70) |
Comments:
ICDD 8-326 (synthetic)
Geological Environment
Geological Setting:
A secondary mineral of uranium mineral deposits.
Type Occurrence of Trögerite
Place of Conservation of Type Material:
Mining Academy, Freiberg, Germany: #21800. Harvard University, Cambridge, Massachusetts, USA: #106035.
Geological Setting of Type Material:
Oxidised zone of a silver-nickel-arsenic-uranium deposit.
Associated Minerals at Type Locality:
Synonyms of Trögerite
Other Language Names for Trögerite
Relationship of Trögerite to other Species
Member of:
Other Members of this group:
Abernathyite | K(UO2)(AsO4) · 3H2O | Tet. 4/mmm (4/m 2/m 2/m) : P4/ncc |
Chernikovite | (H3O)2(UO2)2(PO4)2 · 6H2O | Tet. |
Lehnerite | Mn2+(UO2)2(PO4)2 · 8H2O | Mon. |
Meta-ankoleite | K2(UO2)2(PO4)2 · 6H2O | Tet. 4/mmm (4/m 2/m 2/m) : P4/nmm |
Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O | Tet. 4/mmm (4/m 2/m 2/m) |
Metaheinrichite | Ba(UO2)2(AsO4)2 · 8H2O | Tet. 4mm |
Metakahlerite | Fe2+(UO2)2(AsO4)2 · 8H2O | Tric. 1 : P1 |
Metakirchheimerite | Co(UO2)2(AsO4)2 · 8H2O | Tric. 1 : P1 |
Metalodèvite | Zn(UO2)2(AsO4)2 · 10H2O | Tet. 4/m : P42/m |
Metanatroautunite | Na(UO2)(PO4)(H2O)3 | Tet. 4/mmm (4/m 2/m 2/m) : P4/ncc |
Metanováčekite | Mg(UO2)2(AsO4)2 · 8H2O | Tet. 4/m : P4/n |
Metasaléeite | Mg(UO2)2(PO4)2 · 8H2O | |
Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O | Tet. 4/m : P4/n |
Metauranocircite-I | Ba(UO2)2(PO4)2 · 7H2O | Mon. 2 : P21 |
Metauranospinite | Ca(UO2)2(AsO4)2 · 8H2O | Tet. 4/m : P42/n |
Metazeunerite | Cu(UO2)2(AsO4)2 · 8H2O | Tet. 4/m : P42/n |
Natrouranospinite | Na2(UO2)2(AsO4)2 · 5H2O | Tet. 4/mmm (4/m 2/m 2/m) : P4/nmm |
Uramarsite | (NH4)(UO2)(AsO4) · 3H2O | Tet. 4/mmm (4/m 2/m 2/m) : P4/mmm |
Uramphite | (NH4)2(UO2)2(PO4)2 · 6H2O | Tet. |
Common Associates
Associated Minerals Based on Photo Data:
3 photos of Trögerite associated with Asselbornite | Pb(BiO)3(UO2)4(AsO4)2(OH)7 · 4H2O |
2 photos of Trögerite associated with Metazeunerite | Cu(UO2)2(AsO4)2 · 8H2O |
2 photos of Trögerite associated with Zeunerite | Cu(UO2)2(AsO4)2 · 12H2O |
2 photos of Trögerite associated with Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
1 photo of Trögerite associated with Churchite-(Y) | Y(PO4) · 2H2O |
1 photo of Trögerite associated with Strengite | FePO4 · 2H2O |
Related Minerals - Nickel-Strunz Grouping
8.EB.05 | Autunite | Ca(UO2)2(PO4)2 · 10-12H2O | Orth. mmm (2/m 2/m 2/m) : Pnma |
8.EB.05 | Heinrichite | Ba(UO2)2(AsO4)2 · 10H2O | Mon. 2/m |
8.EB.05 | Kahlerite | Fe(UO2)2(AsO4)2 · 12H2O | Tet. 4/m : P42/n |
8.EB.05 | Nováčekite-I | Mg(UO2)2(AsO4)2 · 12H2O | Tric. 1 : P1 |
8.EB.05 | Saléeite | Mg(UO2)2(PO4)2 · 10H2O | Mon. 2/m |
8.EB.05 | Torbernite | Cu(UO2)2(PO4)2 · 12H2O | Tet. 4/mmm (4/m 2/m 2/m) : I4/mmm |
8.EB.05 | Uranocircite | Ba(UO2)2(PO4)2 · 10H2O | Tet. |
8.EB.05 | Uranospinite | Ca(UO2)(AsO4)2 · 10H2O | Tet. 4/mmm (4/m 2/m 2/m) : P4/nmm |
8.EB.05 | Xiangjiangite | (Fe3+,Al)(UO2)4(PO4)2(SO4)2(OH) · 22H2O | Tet. |
8.EB.05 | Zeunerite | Cu(UO2)2(AsO4)2 · 12H2O | Tet. 4/mmm (4/m 2/m 2/m) : I4/mmm |
8.EB.05 | Metarauchite | Ni(UO2)2(AsO4)2 · 8H2O | Tric. 1 : P1 |
8.EB.05 | Rauchite | Ni(UO2)2(AsO4)2 · 10H2O | Tric. 1 : P1 |
8.EB.10 | Bassetite | Fe2+(UO2)2(PO4)2 · 10H2O | Mon. 2/m |
8.EB.10 | Lehnerite | Mn2+(UO2)2(PO4)2 · 8H2O | Mon. |
8.EB.10 | Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O | Tet. 4/mmm (4/m 2/m 2/m) |
8.EB.10 | Metasaléeite | Mg(UO2)2(PO4)2 · 8H2O | |
8.EB.10 | Metauranocircite-I | Ba(UO2)2(PO4)2 · 7H2O | Mon. 2 : P21 |
8.EB.10 | Metauranospinite | Ca(UO2)2(AsO4)2 · 8H2O | Tet. 4/m : P42/n |
8.EB.10 | Metaheinrichite | Ba(UO2)2(AsO4)2 · 8H2O | Tet. 4mm |
8.EB.10 | Metakahlerite | Fe2+(UO2)2(AsO4)2 · 8H2O | Tric. 1 : P1 |
8.EB.10 | Metakirchheimerite | Co(UO2)2(AsO4)2 · 8H2O | Tric. 1 : P1 |
8.EB.10 | Metanováčekite | Mg(UO2)2(AsO4)2 · 8H2O | Tet. 4/m : P4/n |
8.EB.10 | Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O | Tet. 4/m : P4/n |
8.EB.10 | Metazeunerite | Cu(UO2)2(AsO4)2 · 8H2O | Tet. 4/m : P42/n |
8.EB.10 | Przhevalskite | Pb2(UO2)3(PO4)2(OH)4 · 3H2O | Orth. |
8.EB.10 | Meta-lodèvite | Zn(UO2)2(AsO4)2 · 10H2O | |
8.EB.15 | Abernathyite | K(UO2)(AsO4) · 3H2O | Tet. 4/mmm (4/m 2/m 2/m) : P4/ncc |
8.EB.15 | Chernikovite | (H3O)2(UO2)2(PO4)2 · 6H2O | Tet. |
8.EB.15 | Meta-ankoleite | K2(UO2)2(PO4)2 · 6H2O | Tet. 4/mmm (4/m 2/m 2/m) : P4/nmm |
8.EB.15 | Natrouranospinite | Na2(UO2)2(AsO4)2 · 5H2O | Tet. 4/mmm (4/m 2/m 2/m) : P4/nmm |
8.EB.15 | Uramphite | (NH4)2(UO2)2(PO4)2 · 6H2O | Tet. |
8.EB.15 | Uramarsite | (NH4)(UO2)(AsO4) · 3H2O | Tet. 4/mmm (4/m 2/m 2/m) : P4/mmm |
8.EB.20 | Threadgoldite | Al(UO2)2(PO4)2(OH) · 8H2O | Mon. |
8.EB.20 | Chistyakovaite | Al(UO2)2(AsO4)2(F,OH) · 6.5H2O | Mon. |
8.EB.25 | Arsenuranospathite | Al(UO2)2(AsO4)2F · 20H2O | Orth. mm2 : Pnn2 |
8.EB.25 | Uranospathite | (Al,◻)(UO2)2(PO4)2F · 20(H2O,F) | Orth. mm2 : Pnn2 |
8.EB.30 | Vochtenite | (Fe2+,Mg)Fe3+(UO2)4(PO4)4(OH) · 12-13H2O | Mon. |
8.EB.35 | Coconinoite | Fe3+2Al2(UO2)2(PO4)4(SO4)(OH)2 · 20H2O | Mon. |
8.EB.40 | Ranunculite | HAl(UO2)(PO4)(OH)3 · 4H2O | Mon. |
8.EB.45 | Triangulite | Al3(UO2)4(PO4)4(OH)5 · 5H2O | Tric. |
8.EB.50 | Furongite | Al13(UO2)7(PO4)13(OH)14 · 58H2O | Tric. 1 : P1 |
8.EB.55 | Sabugalite | HAl(UO2)4(PO4)4 · 16H2O | Mon. 2/m : B2/m |
Related Minerals - Hey's Chemical Index of Minerals Grouping
20.7.2 | Natrouranospinite | Na2(UO2)2(AsO4)2 · 5H2O | Tet. 4/mmm (4/m 2/m 2/m) : P4/nmm |
20.7.3 | Abernathyite | K(UO2)(AsO4) · 3H2O | Tet. 4/mmm (4/m 2/m 2/m) : P4/ncc |
20.7.4 | Metazeunerite | Cu(UO2)2(AsO4)2 · 8H2O | Tet. 4/m : P42/n |
20.7.5 | Zeunerite | Cu(UO2)2(AsO4)2 · 12H2O | Tet. 4/mmm (4/m 2/m 2/m) : I4/mmm |
20.7.6 | Metanováčekite | Mg(UO2)2(AsO4)2 · 8H2O | Tet. 4/m : P4/n |
20.7.7 | Nováčekite-I | Mg(UO2)2(AsO4)2 · 12H2O | Tric. 1 : P1 |
20.7.8 | Arsenuranylite | Ca(UO2)4(AsO4)2(OH)4 · 6H2O | Orth. |
20.7.9 | Metauranospinite | Ca(UO2)2(AsO4)2 · 8H2O | Tet. 4/m : P42/n |
20.7.10 | Uranospinite | Ca(UO2)(AsO4)2 · 10H2O | Tet. 4/mmm (4/m 2/m 2/m) : P4/nmm |
20.7.11 | Metaheinrichite | Ba(UO2)2(AsO4)2 · 8H2O | Tet. 4mm |
20.7.12 | Heinrichite | Ba(UO2)2(AsO4)2 · 10H2O | Mon. 2/m |
20.7.13 | Metalodèvite | Zn(UO2)2(AsO4)2 · 10H2O | Tet. 4/m : P42/m |
20.7.14 | Arsenuranospathite | Al(UO2)2(AsO4)2F · 20H2O | Orth. mm2 : Pnn2 |
20.7.15 | Hallimondite | Pb2(UO2)(AsO4)2 · nH2O | Tric. 1 : P1 |
20.7.16 | Hügelite | Pb2(UO2)3(AsO4)2O2 · 5H2O | Mon. |
20.7.17 | Asselbornite | Pb(BiO)3(UO2)4(AsO4)2(OH)7 · 4H2O | Iso. |
20.7.18 | Metakahlerite | Fe2+(UO2)2(AsO4)2 · 8H2O | Tric. 1 : P1 |
20.7.19 | Kahlerite | Fe(UO2)2(AsO4)2 · 12H2O | Tet. 4/m : P42/n |
20.7.20 | Metakirchheimerite | Co(UO2)2(AsO4)2 · 8H2O | Tric. 1 : P1 |
Fluorescence of Trögerite
Lemon-yellow (UV).
Other Information
Notes:
Soluble in acids.
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
References for Trögerite
Reference List:
Sort by Year (asc) | by Year (desc) | by Author (A-Z) | by Author (Z-A)
Weisbach A. (1871), Vorläufige Mitteilung [Über Trögerit und Walpurgin].- Neues Jahrbuch für Mineralogie, Geologie und Paläontologie, 869-870.
Schrauf (1872) Mineralogische und petrographische Mitteilungen, Vienna: 185.
Weisbach A. (1873), Neue Uranerze von Neustädtel bei Schneeberg.- Jahrbuch für das Berg- und Hüttenwesen im Königreiche Sachsen, Abhandlungen, 119-121.
Winkler (1873) Journal für praktische Chemie, Leipzig: 7: 7.
Goldschmidt (1899) Zeitschrift für Kristallographie, Mineralogie und Petrographie, Leipzig: 31: 468.
Larsen, E.S. (1921) The Microscopic Determination of the Nonopaque Minerals, First edition, USGS Bulletin 679: 145
Palache, C., Berman, H., & Frondel, C. (1951), The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana, Yale University 1837-1892, Volume II. John Wiley and Sons, Inc., New York, 7th edition, revised and enlarged, 1124 pp.: 966-967 (as Troegerite).
American Mineralogist (1953): 38: 1159-1168.
Weiss, A., F. Taborszky, K. Hartl, and E. Tröger (1957) Zur Kenntnis des Uranminerals Trögerit. Zeits. Naturforsch., 12b, 356–358.
Frondel, C. (1958) Systematic mineralogy of uranium and thorium. U.S. Geological Survey Bull. 1064, 187–191.
American Mineralogist (1965): 50: 1-12.
Shchipanova, O. V.; Belova, L. N.; Pribytkov, P. V.; Katargina, A. P. (1971): Structure and diagnostics of troegerite and hydrogen-containing uranospinite. Doklady Akademii Nauk SSSR 197, 178-181 (in Russian). [English version: 109-111(?)]
American Mineralogist (1974): 59:763.
Journal of Crystal Growth (1983) 61:606
Gaines, Richard V., H. Catherine W. Skinner, Eugene E. Foord, Brian Mason, Abraham Rosenzweig, and Vandall T. King (1997), Dana's New Mineralogy : The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana: 777.
Chernorukov, N. G.; Nipruk, O. V.; Knyazev, A. V.; Pykhova, Yu. P. (2011): Synthesis and study of uranyl arsenate (UO2)3(AsO4)2 12H2O. Russian Journal of Inorganic Chemistry 56, 163-167. [synth. trögerite]
Internet Links for Trögerite
mindat.org URL:
https://www.mindat.org/min-4013.html
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Localities for Trögerite
Locality List




All localities listed without proper references should be considered as questionable.
Australia | |
| Hurtig, N. C., Heinrich, C. A., Driesner, T., Herrmann, W., Wall, V., & Mathison, I. (2014). Fluid evolution and uranium (-Mo-F) mineralization at the Maureen Deposit (Queensland, Australia): unconformity-related hydrothermal ore formation with a source in the volcanic cover Sequence. Economic Geology, 109(3), 737-773. |
Canada | |
| No reference listed |
Czech Republic | |
| Pauliš P., Kopecký S., Černý P. 2007: Uranové minerály České Republiky a jejich naleziště. 1. část. (Kutna Hora, issue 1) |
| Lapis 2002(7/8), 63-65 |
| Scharm, B.: Přehled minerálů nalezených v oblasti uranových koncentrací v severočeské křídě. Bulletin mineralogicko-petrografického oddělení Národního muzea v Praze, 1995, roč. 3, s. 169-172. |
| Pauliš P., Kopecký S., Černý P. 2007: Uranové minerály České Republiky a jejich naleziště. 1. část. (Kutna Hora, issue 1) |
| Pauliš P., Kopecký S., Černý P. 2007: Uranové minerály České Republiky a jejich naleziště. 1. část. (Kutna Hora, issue 1) |
France | |
| Le Règne Minéral, Hors Série IV (1998) |
| Caubel, A. (1997) Minéralogie du gisement d'uranium de Rabejac (Hérault). Le Règne Minéral: 13: 5-18. |
Germany | |
| Wittern: "Mineralfundorte in Deutschland", 2001 |
| S Wolfsried collection |
Lapis 30(7/8):41-70 (2005) | |
| A. Weisbach (1871): Vorläufige Mittheilung [Über Trögerit und Walpurgin].- Neues Jahrbuch für Mineralogie, Geologie und Paläontologie, 869-870; Palache, C., Berman, H., & Frondel, C. (1951), The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana, Yale University 1837-1892, Volume II: 967, 991. |
| T. Witzke & F. Rüger: Lapis 1998(7/8), 26-64 |
Kazakhstan | |
| Chukanov, N. V., Sidorenko, G. A., Naumova, I. S., Zadov, A. E., Kuz’min, V. I. (2006): Chistyakovaite, a new mineral Al(UO2)2(AsO4)2(F,OH)·6.5H2O. Transactions (Doklady) of the Russian Academy of Sciences/Earth Science Section 407, 290-293 |
Poland | |
| Siuda, R., Gołębiowska, B. (2003): Nowe dane o minerałach wietrzeniowych złoża Miedzianka-Ciechanowice w Rudawach Janowickich (Dolny Śląsk, Polska). Przegląd Geologiczny: 59(3): 226-252 (in Polish) |
Russia | |
| Krinov D.I., Azarova Y.V., Struzhkov S.F., Natalenko M.V., Radchenko Y.I. (2011) On the Discovery of Rooseveltite, Preisingerite, Troegerite, and Zeunerite In Bi-As-Cu-U-mineralization from the Oranzhevoye Ore Field, Verkhne-Kalganinsky Massif, Magadan Region, Russia. New Data on Minerals 46:20-24 |
| Pavel M. Kartashov analytical data 2012 |
Slovakia | |
| Koděra, M. et al., 1986 a 1990 : Topografická mineralógia Slovenska, diel 1- 3, Veda – Vydavateľstvo SAV, Bratislava, 1990, 1 – 1590k |
| Koděra, M. et al., 1986 a 1990 : Topografická mineralógia Slovenska, diel 1- 3, Veda – Vydavateľstvo SAV, Bratislava, 1990, 1 – 1590k |
Spain | |
| http://mineralsabella.blogspot.de/2009/11/minerales-raros-de-uranio.html |
UK | |
| [Journal of the Russell Society, 6(1), 17-26 (1995)] |
| Golley, P. & Williams, R. (1995): Cornish Mineral Reference Manual. Endsleigh Publications (Truro), 104 pp. |
USA | |
| www.cannonmicroprobe.com/Mineral_Specimens.htm |
| SDSMT Bull 18 Roberts and Rapp "Mineralogy of the Black Hills" |
| USGS 1970 PP495-C Cenozoic geology of the Granite Mountains area, central Wyoming |
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