Carminite

Carminite
Carminite from the Alto das Quelhas do Gestoso Mines, Gestoso, Manhouce, São Pedro do Sul, Viseu District, Portugal. Picture width 1.5 mm.
General
CategoryArsenate minerals
Formula
(repeating unit)
PbFe3+2(AsO4)2(OH)2
IMA symbolCmt[1]
Strunz classification8.BH.30 (10 ed)
7/B.28-40 (8 ed)
Dana classification41 Anhydrous phosphates, arsenates and vanadates containing hydroxyl or halogen
Crystal systemOrthorhombic
Crystal classDipyramidal (mmm)
H-M symbol: (2/m 2/m 2/m)
Space groupCccm
Unit cella = 16.591 Å,
b = 7.58 Å,
c = 12.285 Å; Z = 8
Identification
Formula mass639.87 g/mol
ColourCarmine red
Crystal habitTypically bladed crystals, also acicular crystals, in spherical or tufted aggregates and as fibrous or drusy masses
CleavageDistinct on {110}
TenacityBrittle (D, All)
Mohs scale hardness3+12
LustreVitreous, pearly on cleavages
StreakReddish yellow
DiaphaneityTranslucent
Specific gravity5.03–5.18
Optical propertiesBiaxial (+)
Refractive indexnα = 2.070, nβ = 2.070, nγ = 2.080
Birefringence0.010
Pleochroismstrong, X= pale yellowish red; Y=Z= dark carmine red
SolubilitySlowly soluble in HCl with the separation of PbCl2, and totally soluble in HNO3
Other characteristicsCarminite is not radioactive. No piezoelectric effect could be detected[2]
References[3][4][5][6][7]
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Carminite from the Alto das Quelhas do Gestoso Mines, Gestoso, Manhouce, São Pedro do Sul, Viseu District, Portugal. Picture width 8 mm
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Blue scorodite crystals on red brown carminite from Alto das Quelhas do Gestoso Mines, Gestoso, Manhouce, São Pedro do Sul, Viseu District, Portugal. Picture width 3 mm.

Carminite (PbFe3+2(AsO4)2(OH)2[8]) is an anhydrous arsenate mineral containing hydroxyl.[citation needed] It is a rare secondary mineral that is structurally related to palermoite (Li2SrAl4(PO4)4(OH)4).[8] Sewardite (CaFe3+2(AsO4)2(OH)2) is an analogue of carminite, with calcium in sewardite in place of the lead in carminite. Mawbyite is a dimorph (same formula, different structure) of carminite; mawbyite is monoclinic and carminite is orthorhombic.[4] It has a molar mass of 639.87 g.[5] It was discovered in 1850[4] and named for the characteristic carmine colour.[5][6]

  1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  2. ^ Rosenzweig, A and Finney, J J Finney (1959) American Mineralogist 44: 663–665
  3. ^ Mineralienatlas
  4. ^ a b c Carminite on Mindat.org
  5. ^ a b c Carminite data on Webmineral
  6. ^ a b Carminite in the Handbook of Mineralogy
  7. ^ Gaines et al (1997) Dana's New Mineralogy, Eighth Edition. Wiley
  8. ^ a b "Commission on New Minerals, Nomenclature and Classification". Archived from the original on 2011-12-29. Retrieved 2014-09-19.