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Fassinaite
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Lombardo 2 Mine, Monte Trisa Mines, Mercanti Valley, Torrebelvicino, Vicenza Province, Veneto, Italy
© Antonio Zordan
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| System: | Orthorhombic | Colour: | Colourless, white | |||||||||||||||||
| Hardness: | 1½ - 2 | |||||||||||||||||||
| Name: | Named after Bruno Fassina (b. 1943) Italian mineral collector, who discovered the mineral at the Trentini mine in 2009. | |||||||||||||||||||
Classification of Fassinaite | ||||||||||||||||||||||||||||
| IMA status: | Approved 2011 | |||||||||||||||||||||||||||
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| mindat.org URL: | http://www.mindat.org/min-40169.html Please feel free to link to this page. | |||||||||||||||||||||||||||
Type Occurrence of Fassinaite | ||||||||||||||||||||||||||||
| Type Locality: | Trentini Mine (Beata Maria Vergine Mine), Contrada Trentini, Torrebelvicino, Vicenza Province, Veneto, Italy | |||||||||||||||||||||||||||
| General Appearance of Type Material: | Radiating aggregates of acicular, colourless crystals up to 0.2 mm long. | |||||||||||||||||||||||||||
| Place of Conservation of Type Material: | Museum of Mineralogy of the Department of Geosciences at the University of Padova, Italy, under catalogue number MMP M10008. | |||||||||||||||||||||||||||
| Geological Setting of type material: | The mineralization is linked to Mid-Triassic calc-alkaline magmatism. Hydrothermal fluids related to volcanism deposited sulphides, baryte and Fe- and Mn-bearing minerals at the boundary between Ladinic volcanites and limestone of the Mount Spitz Formation. Supergene minerals including sulphates, carbonates and arsenates of Zn, Pb and Cu are very common. | |||||||||||||||||||||||||||
Physical Properties of Fassinaite | ||||||||||||||||||||||||||||
| Lustre: | Adamantine | |||||||||||||||||||||||||||
| Diaphaneity (Transparency): | Transparent, Translucent | |||||||||||||||||||||||||||
| Colour: | Colourless, white | |||||||||||||||||||||||||||
| Streak: | White | |||||||||||||||||||||||||||
| Hardness (Mohs): | 1½ - 2 | |||||||||||||||||||||||||||
| Hardness Data: | Estimated | |||||||||||||||||||||||||||
| Tenacity: | Brittle | |||||||||||||||||||||||||||
| Cleavage: | None Observed | |||||||||||||||||||||||||||
| Fracture: | Irregular/Uneven | |||||||||||||||||||||||||||
| Density (calculated): | 6.084 g/cm3 | |||||||||||||||||||||||||||
Crystallography of Fassinaite | ||||||||||||||||||||||||||||
| Crystal System: | Orthorhombic | |||||||||||||||||||||||||||
| Class (H-M): | mmm (2/m 2/m 2/m) - Dipyramidal | |||||||||||||||||||||||||||
| Space Group: | Pnma {P21/n 21/m 21/a} | |||||||||||||||||||||||||||
| Cell Parameters: | a = 16.343(1) Å, b = 8.760(2) Å, c = 4.592(3) Å | |||||||||||||||||||||||||||
| Ratio: | a:b:c = 1.866 : 1 : 0.524 | |||||||||||||||||||||||||||
| Unit Cell Volume: | V 657.4 ų | |||||||||||||||||||||||||||
| Z: | 2 | |||||||||||||||||||||||||||
| Morphology: | The crystals are acicular to prismatic [010], with a flattened diamond-shaped cross-section. The Austrian crystals are sufficiently well developed to allow determination of some of the crystal forms: the prism {101} is large and dominant, with a flat chisel-shaped {hk0} termination, possibly {110}. Small faces which are possibly {011} are rarely present. Further forms are minute and difficult to measure as they are commonly rounded. | |||||||||||||||||||||||||||
| Twinning: | None observed. | |||||||||||||||||||||||||||
| X-Ray Powder Diffraction: |
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Chemical Properties of Fassinaite | ||||||||||||||||||||||||||||
| Formula: |
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| Essential elements: | C, O, Pb, S | |||||||||||||||||||||||||||
| All elements listed in formula: | C, O, Pb, S | |||||||||||||||||||||||||||
| Analytical Data: | Average of 11 electron microprobe analyses (CO2 calculated from the stoichiometry).PbO (77.1) SO3 (12.0) CO2 (7.60) S(2-) (4.83) O=S(2-) (-2.41) Total (99.2) | |||||||||||||||||||||||||||
| Empirical Formula: |
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Other Names for Fassinaite | ||||||||||||||||||||||||||||
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Other Information | ||||||||||||||||||||||||||||
| Health Warning: | No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care. | |||||||||||||||||||||||||||
References for Fassinaite | ||||||||||||||||||||||||||||
| Reference List: - + | U. Kolitsch (2010): Pb2(S2O3)(CO3): The first naturally occurring thiosulphate carbonate and its atomic arrangement. Oral presentation, 20th General Meeting of the IMA (IMA2010), Budapest, Hungary, August 21-27; abstract in CD of Abstracts, p. 489. Nestola, F., Bindi, L., Guastoni, A., Zorzi, F., Nasdala, L. (2011): Pb2(CO3)(S2O3), the first mineral with coexisting carbonate and thiosulfate groups from Trentini mine, Vicenza, Italy. Poster, Geoitalia 2011, Turin, Italy, September 19-23, 2011; abstract in Plinius 37, 308. Bindi, L., Nestola, F., Guastoni, A., Zorzi, F. and Nasdala, L. (2011): Fassinaite, IMA 2011-048. CNMNC Newsletter No. 10, 2559. Bindi, L., Nestola, F., Kolitsch, U., Guastoni, A. & Zorzi, F. (2011): Fassinaite, Pb2+2(S2O3)(CO3), the first mineral with coexisting thiosulphate and carbonate groups: description and crystal structure. Mineralogical Magazine, 75, 2721-2732. U. Kolitsch, L. Bindi, F. Nestola, A. Guastoni, F. Zorzi and R. Poeverlein (2012): Fassinait, ein neues Bleimineral aus Italien, Österreich und Deutschland. Lapis 37 (1), 52-53; 62 (in German). | |||||||||||||||||||||||||||
Internet Links for Fassinaite | ||||||||||||||||||||||||||||
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Localities for Fassinaite | ||||||||||||||||||||||||||||
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(TL) indicates type locality. ? indicates mineral may be doubtful at this locality. All other localities listed without reference should be considered as uncertain and unproven until references can be found.
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New Locality Added: Ajmal Mine, Kechau Tui, Pahang, MalaysiaFrom David Von Bargen, 21st May 2013 20:41:31

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