Mawbyite | |
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General | |
Category | Mineral |
Formula (repeating unit) | Pb(Fe3+,Zn)2(AsO4)2(OH)2 |
IMA symbol | Mby |
Strunz classification | 08.CG.15 |
Dana classification | 40.02.09.04 |
Crystal system | Monoclinic |
Crystal class | Prismatic H-M Symbol: 2/m |
Space group | B2/m |
Unit cell | 391.13 |
Identification | |
Formula mass | 649.02 |
Color | Pale brown to orange-brown to bright reddish brown |
Crystal habit | Spherical or wheat sheaf shaped crystals |
Twinning | Common, V-shaped at about {100} |
Cleavage | Good on {001} |
Fracture | Conchoidal |
Mohs scale hardness | 4 |
Luster | Adamantine |
Streak | Orange-yellow |
Diaphaneity | Transparent to Translucent |
Specific gravity | 5.365 |
Density | 5.5 |
Optical properties | Biaxial (−) |
Refractive index | nα = 1.940(2) nβ = 2.000(2) nγ = 2.040(2) |
Birefringence | 0.100 |
Pleochroism | Weak Brown to reddish brown |
2V angle | Measured: 80° (5) Calculated: 76° |
Dispersion | Relatively weak |
Length fast/slow | Length-fast |
Ultraviolet fluorescence | None |
Mawbyite is a lead iron zinc arsenate that was named in honor of Maurice Alan Edgar Mawby. It has been approved by the IMA in 1988, and was published just a year after being described by Pring. Mawbyite is a member of the tsumcorite group, the monoclinic dimorph of carminite.[1] It was first believed to be tsumcorite; however, crystal-structure determination showed iron and zinc occupying the same crystallographic site instead,[2] and through the analysis it turned out mawbyite is isostructural with tsumcorite, meaning the two share a similar formula. More accurately, mawbyite appears to be the ferric analogue of the aforementioned mineral.[3] The relationship between helmutwinklerite – which shares a similar formula with tsumcorite's – and mawbyite had been suggested, but due to lack of data it remains unclear. A full crystal-structure analysis is required in order to understand the relationship between their structures.[2]
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