Tsumcorite

Tsumcorite

Tsumcorite from the Tsumeb Mine, Namibia
General
Category Arsenate minerals
Formula
(repeating unit)		 PbZnFe2+(AsO4)2.H2O
Strunz classification 8.CG.15
Dana classification 40.02.09.01
Crystal system Monoclinic
Unit cell a = 9.124 Å, b = 6.329 Å
c = 7.577 Å; β = 115.3°; Z = 2
Identification
Formula mass 624.29 g
Color Yellow-brown, red-brown, orange
Crystal habit Radiating, fibrous crusts
Crystal symmetry Monoclinic - prismatic
H-M symbol (2/m)
Twinning Common, on a unknown law
Cleavage Good on {001}
Mohs scale hardness 4½
Luster Vitreous
Streak Yellow
Diaphaneity Translucent
Specific gravity 5.2
Optical properties Biaxial
Refractive index nα = 1.87–1.91 nβ = 1.89–1.93 nγ = 1.92–1.96
Pleochroism Weak, yellow to yellow-green
2V angle 67–83.5°
Solubility Dissolves in HCl
References [1][2][3][4][5]

Tsumcorite is a rare hydrated lead arsenate mineral that was discovered in 1971, and reported by Geier, Kautz and Muller.[5] It was named after the TSUMeb CORporation mine at Tsumeb, in Namibia, in recognition of the Corporation’s support for mineralogical investigations of the orebody at its Mineral Research Laboratory.[4]

Unit cell

Tsumcorite belongs to the monoclinic crystal class 2/m, which means that it has a twofold axis of symmetry along the b axis and a mirror plane perpendicular to this, in the plane containing the a and c axes. The a and c axes are inclined to each other at angle β = 115.3°. The unit cell parameters are a = 9.124 Å to 9.131 Å, b = 6.326 Å to 6.329 Å and c = 7.577 Å to 7.583 Å.[1][2][3][5] There are two formula units per unit cell (Z = 2), and the space group is C2/m, meaning that the cell is a C-face centred lattice, with lattice points in the center of the C face as well as at the corners of the cell.[6] The structure is related to the brackebushite group structure.[1]

Mineral series

Tsumcorite belongs to the helmutwinklerite group,[1] whose members are

Tsumcorite forms a series with helmutwinklerite as Zn replaces the Fe2+, with thometzekite as Cu replaces the Zn and Fe2+,[1][3] and also with mawbyite.[7]

Crystal habit and properties

Crystals are prismatic, elongated along the b axis, or wedge-shaped. They occur in radiating sheaves and spherulites, and as fibrous crusts or earthy and powdery material.[4] Cleavage is good perpendicular to the c axis,[4] and twinning is common.[4]

Tsumcorite is yellow-brown, red-brown or orange in color, and it is one of the few minerals that have a yellow streak (orpiment and crocoite are two others). It is translucent, with a vitreous luster, and dichroic yellow to yellow-green.[1][5] The optical class is biaxial and the refractive indices are approximately equal to 1.90.[1][3][5]

The mineral is moderately hard, with a Mohs hardness of 4½, between fluorite and apatite,[1][2][3][4] and quite heavy, due to the lead content, with specific gravity 5.2, which is more than baryte but less than cerussite. It dissolves in hydrochloric acid[1][5] and it is not radioactive.[3]

Occurrence and associations

Tsumcorite is a rare secondary mineral in the oxidized zone of some arsenic-bearing hydrothermal lead-zinc deposits.[1][4][5]

The type locality is the Tsumeb Mine, Tsumeb, Otjikoto Region, Namibia, where it is associated with willemite, smithsonite, mimetite, scorodite, anglesite, arseniosiderite, beaverite, beudantite, carminite, ludlockite, o’danielite, zincroselite, stranskiite and leiteite.[4] At the Puttapa Mine in Australia it occurs with adamite, mimetite, smithsonite, goethite and quartz.[4] At the Kintore Open Cut, Broken Hill, Australia it occurs with segnitite, beudantite, carminite and mawbyite.[7]

References

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  1. 1 2 3 4 5 6 7 8 9 10 Gaines et al (1997) Dana’s New Mineralogy Eighth Edition. Wiley
  2. 1 2 3 Mindat.org
  3. 1 2 3 4 5 6 Webmineral data
  4. 1 2 3 4 5 6 7 8 9 Handbook of Mineralogy
  5. 1 2 3 4 5 6 7 Fleischer M (1972) New mineral names, American Mineralogist 57, 1558, being a summary of Geier, Kautz and Muller (1971) Neues Jahrbuch fur Mineralogie (Monatshefte) 1971: 304-309
  6. ↑ Crystallography (1993) Walter Borchardt-Ott, Springer Verlag
  7. 1 2 Australian Journal of Mineralogy (1997) 3-1:62
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