Hureaulite Explained

Boxbgcolor:
  1. d0a280
Hureaulite
Category:Phosphate minerals
Imasymbol:Hur[1]
Molweight:728.65 g/mol
Strunz:8.CB.10 (10 ed)
7/C.04-10 (8 ed)
Dana:39.2.1.1
System:Monoclinic
Class:Prismatic (2/m)
(same H-M symbol)
Symmetry:C2/c
Unit Cell:a = 17.594(10) Å
b = 9.086(5) Å
c = 9.404(5) Å
β = 96.67(8)°; Z = 4
Colour:Orange, red, yellow, brown, grey or nearly colourless
Habit:Crystals are short prismatic parallel to (100) or equant, sometimes thick tabular, also massive or imperfectly fibrous[2]
Cleavage: good
Fracture:Uneven
Tenacity:Brittle
Mohs:3.5
Lustre:Vitreous to greasy
Refractive:nα = 1.640 – 1.654 nβ = 1.649 – 1.659 nγ = 1.655 – 1.662
Opticalprop:Biaxial (−)
2V:greater than 60°
Dispersion:r
Birefringence:δ = 0.012
Pleochroism:X colourless, Y yellow to pale rose, Z reddish yellow to reddish brown
Streak:Nearly white
Gravity:3.18–3.2 (measured), 3.23 (calculated)
Solubility:Easily soluble in acids.
Diaphaneity:Transparent to translucent
References:[3] [4] [5] [6]

Hureaulite is a manganese phosphate with the formula . It was discovered in 1825 and named in 1826 for the type locality, Les Hureaux, Saint-Sylvestre, Haute-Vienne, Limousin, France. It is sometimes written as huréaulite, but the IMA does not recommend this for English language text.[7]

A complete series exists from lithiophilite, to triphylite,, including hureaulite, strengite,, stewartite,, and sicklerite, .[8]

Environment

Hureaulite is a secondary mineral occurring in granite pegmatites.[6] At the type locality it occurs in a zone of altered triphylite,, in pegmatite. Typically occurs very late in the sequence of formation of secondary phosphate minerals.[9] Associated at the type locality with vivianite, ; rockbridgeite, ; heterosite, and cacoxenite, . It can be synthesised;[10] most natural hureaulites are Mn-rich compounds but extensive solution is known for synthetic material.[9]

Localities

The type locality is Les Hureaux, Saint-Sylvestre, Haute-Vienne, Limousin, France. Hureaulite is also found in a granite pegmatite known for its phosphates in the Aimorés pegmatite district, at the Cigana claim in Galiléia, Doce valley, Minas Gerais, Brazil, formerly known as the Jocão Mine.[4]

Notes and References

  1. Warr. L.N.. 2021. IMA–CNMNC approved mineral symbols. Mineralogical Magazine. 85. 3. 291–320. 10.1180/mgm.2021.43. 2021MinM...85..291W. 235729616. free.
  2. Murdoch, Joseph (1942) Contributions to the Crystallography of Hureaulite. American Mineralogist 27: 228
  3. Gaines et al (1997) Dana's New Mineralogy Eighth Edition
  4. http://www.mindat.org/min-1952.html Mindat.org
  5. Shigley and Brown (1985) American Mineralogist 70:395
  6. Roberts, Campbell and Rapp (1990) Encyclopedia of Minerals, 2nd edition
  7. Burke, E. A. J. (2008): Tidying up Mineral Names: An IMA scheme for Suffixes, Hyphens and Diacritical Marks. Mineralogical Record, 39, 134
  8. Murdoch, Joseph (1943) Crystallography of Hureaulite. American Mineralogist 28: 19-24
  9. Moore, P B, and Araki, T (1973) Hureaulite: its atomic arrangement. American Mineralogist 58: 302-307.
  10. Gerault, Y, Riou, A, and Cudennec, Y (1987) Acta Crystallographica (C) 43:1829