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Ferdowsiite

A valid IMA mineral species
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About FerdowsiiteHide

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Ferdowsi Tousi
Formula:
Ag8(Sb5As3)S16
A Pb-bearing variety was also described (Makovicky et al., 2013).
Colour:
Greyish black
Lustre:
Metallic
Hardness:
2½ - 3
Specific Gravity:
5.3 (Calculated)
Crystal System:
Monoclinic
Name:
The name is for one of the greatest Persian personalities, Ferdowsi Tousi (935–1020), one of the greatest Persian poets to have ever lived. His life-long endeavor to preserve the national identity, language and heritage of his homeland, especially through one of the greatest poetic masterpieces, the Shahnameh, won him lasting fame and honor.
Superstructure of PbS.

Member of the group of ABX2-type sulfosalts of silver, combining antimony and arsenic, with a crystal structure different from other members of this group.

Related to sangenaroite and ~Sb5As3 analogue of the latter.


Unique IdentifiersHide

Mindat ID:
43594
Long-form identifier:
mindat:1:1:43594:7

IMA Classification of FerdowsiiteHide

Classification of FerdowsiiteHide

2.JA.

2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
J : Sulfosalts of PbS archetype
A : Galena derivatives with little or no Pb

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
FdwIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of FerdowsiiteHide

Metallic
Transparency:
Opaque
Colour:
Greyish black
Streak:
Dark grey
Hardness:
2½ - 3 on Mohs scale
Comment:
estimated
Tenacity:
Brittle
Cleavage:
None Observed
Parting:
None observed
Fracture:
Irregular/Uneven
Density:
5.3 g/cm3 (Calculated)
Comment:
Could not be measured due to lack of material.

Optical Data of FerdowsiiteHide

Anisotropism:
Distinct in air, and further enhanced in oil. Rotation tints vary between dark brown and bluish grey
Bireflectance:
Distinct
Reflectivity:
WavelengthR1 (%)R2 (%)
400nm32.3%37.4%
420nm36.1%38.5%
440nm35.7%37.8%
460nm35.1%37.3%
470nm34.9%37.3%
480nm34.9%37.4%
500nm34.3%37.1%
520nm34.1%36.7%
540nm33.5%36.3%
546nm33.4%35.9%
560nm33.3%35.9%
580nm32.4%35.3%
589nm32.4%35.1%
600nm32.3%35.1%
620nm31.8%34.4%
640nm31.0%33.8%
650nm30.7%33.5%
660nm30.4%33.0%
680nm29.8%32.6%
700nm29.2%31.9%


Graph shows reflectance levels at different wavelengths (in nm). Peak reflectance is 38.5%.
R1 shown in black, R2 shown in red
Colour in reflected light:
Greyish white
Internal Reflections:
Not observable
Pleochroism:
Visible
Comments:
Distinct, white to grey

Chemistry of FerdowsiiteHide

Mindat Formula:
Ag8(Sb5As3)S16

A Pb-bearing variety was also described (Makovicky et al., 2013).
Element Weights:
Element% weight
Ag39.055 %
Sb27.553 %
S23.219 %
As10.172 %

Calculated from ideal end-member formula.
Ag
Sb
S
As

Crystallography of FerdowsiiteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/c
Setting:
P21/n
Cell Parameters:
a = 8.677(2) Å, b = 5.799(1) Å, c = 13.839(3) Å
β = 96.175(4)°
Ratio:
a:b:c = 1.496 : 1 : 2.386
Unit Cell V:
692.28 ų
Z:
1
Morphology:
Elongated crystals

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
High-𝑇 alteration and/or metamorphism
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Type Occurrence of Ferdowsiite