Macphersonite

(repeating unit)Pb4(SO4)(CO3)2 (OH)2IMA symbolMps[1]Strunz classification5.BF.40Dana classification17.01.04.01Crystal systemOrthorhombicCrystal classDipyramidal (mmm)
H-M symbol: (2/m 2/m 2/m)Space groupPcabUnit cella = 10.37 Å, b = 23.10 Å,
c = 9.25 Å,
β = 106.43°; Z = 8IdentificationFormula mass1,078.90 g/molColorWhite, pale amber, colorlessCrystal habitPseudo hexagonal, tabularTwinningPolysynthetic, lamellar, contactCleavagePerfect on {010}FractureUnevenMohs scale hardness2.5 - 3LusterAdamantine, otherwise resinousStreakWhiteSpecific gravity6.50Optical propertiesBiaxial (-)Refractive indexnα = 1.870 nβ = 2.000 nγ = 2.010Birefringenceδ = 0.1402V angle35-36°Dispersionr > vUltraviolet fluorescenceA very strong and vivid yellowOther characteristicsPolymorph of leadhillite and susanniteReferences[2][3][4][5][6]

Macphersonite, Pb4(SO4)(CO3)2 (OH)2, is a carbonate mineral that is trimorphous with leadhillite and susannite. Macphersonite is generally white, colorless, or a pale amber in color and has a white streak. It crystallizes in the orthorhombic system with a space group of Pcab. It is fairly soft mineral that has a high specific gravity.

Macphersonite is named after Harry Gordon Macpherson,[4] a keeper of minerals at the Royal Scottish Museum. It was discovered and accepted in 1984.

Structure

The structure of macphersonite is represented as a sequence of three layers stacked along the [001]. The first layer is a sulfate tetrahedra, the second is of lead and hydroxide, and the third is a layer composed of lead and carbonate. Stacking of the three layers can be detailed as ...BABCCBABCC...[5] similar to leadhillite. Two C layers of lead carbonate in the BAB stacking provide a weak connection that leads to the perfect {001} cleavage.

Physical properties

The Leadhills macphersonite is a very pale amber to colorless in color, while the Argentolle mine macphersonite is colorless to white.[4] It has a luster of adamantine on fresh surfaces and elsewhere it is resinous. Macphersonite is soft with a 2.5-3 on the Mohs hardness, has an uneven fracture with a high density of 6.5g/cm3.[3]

Macphersonite has a very strong yellow fluorescence under both long and short wave, ultraviolet is displayed by the Leadhills specimens, the Argentolle material does not fluoresce.

Occurrence

Macphersonite is found in the Leadhills region of southwest Scotland and in the Saint-Prix, Saône-et-Loire region of France. It is the rarest of the three polymorphs. It occurs in lead deposits associated with cerussite, susannite, caledonite, scotlandite, leadhillite, galena and pyromorphite.

References

  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. ^ Mineralienatlas
  3. ^ a b Web Mineral
  4. ^ a b c Livingstone, A.; Sarp, H. (1984). "Macphersonite, a new mineral from Leadhills, Scotland, and Saint-Prix, France – a polymorph of leadhillite and susannite" (PDF). Mineralogical Magazine. 48 (347): 277–82. Bibcode:1984MinM...48..277L. doi:10.1180/minmag.1984.048.347.14. S2CID 55488942. Retrieved 26 June 2016.
  5. ^ a b Steele, Ian, Pluth, Joseph, Livingstone, Alan. Crystal structure of macphersonite (Pb4(SO4)(CO3)2 (OH)2): comparison with leadhillite Mineralogical Magazine, 1998 vol 62(4), pp 451=459
  6. ^ Macphersonite data on Mindat