Falsterite

Falsterite
General
Category Phosphate mineral
Formula
(repeating unit)
Ca2MgMn2+2(Fe2+0.5Fe3+0.5)4Zn4(PO4)8(OH)4(H2O)14
Crystal system Monoclinic, P21/c
Unit cell a=6.39, b=21.26, c=15.37 [Å], β = 90.56o (approximated)
Identification
Color Greenish-blue
Crystal habit thin plates, rectangular laths
Crystal symmetry Monoclinic (2/m)
Cleavage {010}, perfect
Fracture Uneven
Luster Vitreous
Streak Very pale greenish-blue
Diaphaneity Transparent
Density 2.78 (measured); 2.84 (calculated; approximated)
Optical properties Biaxal (-)
Refractive index nα=1.58, nβ=1.60, nγ=1.61 (approximated)
Pleochroism Colorless to very pale yellow (X & Z), blue-green (Y)
Dispersion Strong
References [1][2]

Falsterite is a rare phosphate mineral[2] wit the formula Ca2MgMn2+2(Fe2+0.5Fe3+0.5)4Zn4(PO4)8(OH)4(H2O)14.[1] It is a pegmatitic mineral, related to the currently approved mineral ferraioloite.[2]

Occurrence and association

Falsterite was found in Palermo No. 1 pegmatite, North Groton, Grafton County, New Hampshire, US. Co-type locality is pegmatite at Estes quarry, Baldwin, Cumberland County, Maine, US. Falsterite is a product of alteration of triphylite and sphalerite.[1]

Crystal structure

Main features of the crystal structure of falsterite, which is somewhat similar to that of schoonerite, are:

The slabs are bridged by dimers of MgO6 octahedra that display edge-sharing. Magnesium-bearing octahedra share edges with zinc-bearing tetrahedra.[1]

References

  1. 1 2 3 4 Kampf, A.R., Mills, S.J., Simmons, W.B., Nizamoff, J.W., and Whitmore, R.W., 2012. Falsterite, Ca2MgMn2+2(Fe2+0.5Fe3+0.5)4Zn4(PO4)8(OH)4(H2O)14, a new secondary phosphate mineral from the Palermo No. 1 pegmatite, North Groton, New Hampshire. American Mineralogist 97(4), 496-502
  2. 1 2 3 "Falsterite: Falsterite mineral information and data". Mindat.org. Retrieved 2016-03-04.
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