Mooihoekite

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Mooihoekite
General
Category Sulfide mineral
Formula
(repeating unit)
Cu9Fe9S16
Strunz classification 02.CB.10b
Crystal symmetry Tetragonal 42m scalenohedral
Unit cell a = 10.58 Å, c = 5.38 Å; volume= 602.22 ų; Z = 1
Identification
Formula mass 1,587.59 g
Color Pale yellow. Tarnishes to pinkish brown and purple
Crystal habit Granular - Generally occurs as anhedral to subhedral crystals in matrix
Crystal system Tetragonal
Mohs scale hardness 4
Luster Metallic
Streak Black
Diaphaneity Opaque
Specific gravity 4.36
Optical properties Weakly anisotropic
References [1][2][3][4][5]

Mooihoekite is a copper iron sulfide mineral with chemical formula of Cu9Fe9S16. The mineral was discovered in 1972 and received its name from its discovery area, the Mooihoek mine in Transvaal, South Africa.[3]

Crystal structure and optical properties[edit]

Mooihoekite crystallizes in the tetragonal crystal system. It has a short optical c-axis that is perpendicular to two longer a-axes of equal length. For Mooihoekite, the c-axis is a 4-fold rotoinversion axis.[1]

Mooihoekite is an opaque mineral which shows weak anisotropism in polished section under reflected light microscopy. It goes slightly extinct every 90°.[1]

Occurrence[edit]

It is found in massive sulfide from pipe-shaped dunite pegmatite in the norite zone of the Bushveld igneous complex in South Africa. It has also been found in troctolite from the basal Duluth gabbro in Minnesota, USA; in the Talnakh area, Norilsk region, western Siberia; at Krzemianka, Poland; in the Malanjkhand copper-molybdenum deposit, Madhya Pradesh, India; and the Stillwater igneous complex in Montana, USA.[5][4]

Mooihoekite occurs in association with haycockite, magnetite, troilite, cuprian pentlandite, mackinawite, sphalerite, and moncheite in the Mooihoek mine and with haycockite, native copper, troilite, pentlandite, cubanite and magnetite in the Duluth complex.[5]

Uses[edit]

Mooihoekite is a rare mineral that is mostly used for research purposes. It has similar properties to chalcopyrite CuFeS2, making it helpful in the study of ore deposits and the study of the central portion of the Cu-Fe-S phase system.[1] Mooihoekite, chalcopyrite, talnakhite, and haycockite all play key roles in the study of ore genesis and beneficiation.

References[edit]

  1. ^ a b c d Cabri, L.J. and Hall, S.R. (1972) Mooihoekite and Haycockite, Two New Copper-Iron Sulfides, and Their Relationship to Chalcopyrite and Talnakhite. American Mineralogist, 57, 689-708.
  2. ^ Hall, S.R. and Rowland, J.F. (1973) The Crystal Structure of Synthetic Mooihoekite. Acta Crystallographica, 29, 2365-2372.
  3. ^ a b Webmineral data
  4. ^ a b Mindat.org
  5. ^ a b c Handbook of Mineralogy