Dessauite-(Y)

Dessauite-(Y)
General
Category Oxide mineral
Crichtonite group
Formula
(repeating unit)
(Sr,Pb)(Y,U)(Ti,Fe3+)20O38
Strunz classification 4.CC.40
Crystal system Trigonal
Crystal class Rhombohedral (3)
H-M symbol: (3)
Space group R3
Unit cell a = 9.197 Å, α = 68.75°
Identification
Formula mass 1,856.57 g/mol
Color Black; ash-grey with pale bluish tones.
Crystal habit Tabular
Cleavage None
Fracture Conchoidal
Tenacity Brittle
Mohs scale hardness 6½ - 7
Luster Metallic luster
Streak Black
Diaphaneity Opaque
Density 4.68 g/cm3 (calculated)
Birefringence Low
Pleochroism Very weak

Dessauite-(Y) is a mineral member of the crichtonite group with the formula (Sr,Pb)(Y,U)(Ti,Fe3+)20O38. It is associated with derbylite, hematite, rutile, karelianite, siderite, and calcite. Founded in the Buca della Vena Mine, Tuscany, Italy, the mineral was called dessauite in honor of professor Gabor Dessau (1907–1983).[1]

Structure

Dessauite occurs as small, flattened rhombohedral crystals, tabular {001} with hexagonal outline. Members of the Crichtonite group may be confused with ilmenite or hematite.[2] The difference between dessauite and other minerals in the crichonite group is the occurrence of three additional octahedral sites and of a site in square pyramidal coordination, all with low occupancies. The mineral is black and opaque, presents a metallic luster, and it is brittle. Dessauite presents dimensions of diameter up to 1mm and thickness up to 0.2mm. In reflected plane-polarized light the color is ash-grey with pale bluish tones.[1] The calculated density is 4.68 g/cm3. The habit is tabular, forming thin dimensions in one direction and hardness of 6.5 and 7.[3] Dessauite differs from other elements of the crichtonite group because of the quantity of cations and X-ray diffraction patter.

Occurrence

Dessauite was found in the Buca della Vena Mine, Apuan Alps, northern Tuscany, Italy, with many other minerals, coming from hydrothermal fluids circulating through a small hematite-barite ore deposit within dolomite, during an alpine metamorphic event. It occurs in calcite veins hosted within dolomite and is associated with calcite, rutile, hematite, siderite, and derbylite.[1]

See also

References

  1. 1 2 3 Orlandi, Paolo (1997). "Dessauite, (Sr,Pb)(Y,U)(Ti,Fe3+)20O38, a new mineral of the crichtonite group from Buca della Vena mine, Tuscany, Italy." (PDF). Journal of the Mineralogical Society of America.
  2. "Crichtonite Group".
  3. "Dessauite Mineral Data". www.webmineral.com. Retrieved 2015-12-02.


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