Samiksha Jaiswal (Editor)

Triplite

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Category
  
Phosphate minerals

Strunz classification
  
8.BB.10

Formula (repeating unit)
  
(Mn,Fe)2(PO4)(F,OH)

Crystal system
  
Monoclinic

Triplite

Crystal class
  
Prismatic (2/m) (same H-M symbol)

Unit cell
  
a = 11.97 Å, b = 6.52 Å c = 10.09 Å; β = 105.62°; Z = 8

Triplite is a rare phosphate mineral with formula: (Mn,Fe)2PO4(F,OH). It occurs in phosphate-rich granitic pegmatites typically as irregular brown opaque masses. Triplite was first described in 1813 for an occurrence in Chanteloube, Limousin, France. The name is from the Greek triplos for triple, in reference to the three cleavage directions. In color and appearance, it is very similar to rhodocrosite, another manganese bearing mineral. Chemically, it is also quite similar to triploidite the difference being that triplite is fluorine dominant while triploidite is hydroxide dominant.

Occurrence

Triplite is a rare fluoro-hydroxide phosphate mineral that forms in phosphate rich granite pegmatites and high temperature hydrothermal veins. It has been found in the United States in California, Nevada, Arizona, Colorado, South Dakota, Virginia, Connecticut, and Maine. Other occurrences include the Shigar Valley, Pakistan; China; Bavaria, Germany; Kimito, Finland and Karibib, Namibia.

References

Triplite Wikipedia