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Miguelromeroite

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Pale pink mineral - synthetic compound
Miguelromeroite
General
CategoryMineral
Formula
(repeating unit)
MnS(AsO4)2(HAsO4)2 · 4H2O
IMA symbolMig
Crystal systemMonoclinic
Crystal classPrismatic
H-M symbol: 2/m
Space groupB2/b
Unit cell1,624.38
Identification
ColorSalmon pink to orange
TwinningNone observed
CleavageGood on {100}
FractureConchoidal
Mohs scale hardness4
LusterVitreous
StreakPale pink
DiaphaneityTransparent
Density3.69
Optical propertiesBiaxial (−)
Refractive indexnα = 1.713
nβ = 1.723
nγ = 1.729
Birefringence0.016
PleochroismVisible
2V angleMeasured: 70°
Calculated: 75°

Miguelromeroite is a mineral named for Miguel Romero Sanchez by Anthony Robert Kampf. The mineral, first described in 2008 was named in 2009, the same year it got approved by the International Mineralogical Association.

Properties

Miguelromeroite is a member of the hureaulite group, and is the magnesium analogue of the mineral sainfeldite. It is known as a synthetic compound, and was originally labeled as villyaellenite due to the very rare complex arsenate microcrystals. It shows pleochroic attributes, which is an optical phenomenon that makes gems to be seen a different color depending on the axis it is being inspected. Viewing it from the Z axis, the mineral can be seen in a pale pink color. It was redefined as an intermediate species of the series. It is the full magnesium endmember of the series. Crystals are up to 4 cms in length, and are elongated on with forms {100}, {110} and {101̅}.

Structure

The mineral's structure is defined by an octahedral edge-sharing pentamer. The pentamers are linked into a loose framework by sharing corners with octahedra in adjacent pentamers and they are further linked through AsO4 and AsO3OH tetrahedra. There are three distinct octahedral sites: M1, M2, and M3. In miguelromeroite's structure, all of the octahedral sites are occupied by magnesium and the average bond lengths for the sites fall within a relatively narrow range. Though the differences in the sites suggest that the sites M2 and M3 contain small amounts of zinc and calcium.

Mines

The samples were from the Veta Negra mine in Chile. Other mines include Gozaisho mine in Honshu island, Japan, and Mina Ojuela in Mapimi, Durango, Mexico. It's a type locality only in these three mines.

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. ^ Minerals, Dakota Matrix. "Miguelromeroite mineral information and data". www.dakotamatrix.com. Retrieved 2021-08-09.
  3. ^ "Miguelromeroite". www.mindat.org. Retrieved 2021-08-09.
  4. ^ R. Kampf, Anthony (2009). "Miguelromeroite, the Mn analogue of sainfeldite, and redefinition of villyaellenite as an ordered intermediate in the sainfeldite-miguelromeroite series" (PDF). American Mineralogist. 94 (11–12): 1535–1540. Bibcode:2009AmMin..94.1535K. doi:10.2138/am.2009.3278. S2CID 97734557.
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