Ferrodimolybdenite
A valid IMA mineral species
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Formula:
FeMo2S4
Colour:
grey
Lustre:
Metallic
Hardness:
3
Specific Gravity:
5.445 (Calculated)
Crystal System:
Monoclinic
Name:
The mineral name ferrodimolybdenite is derived from its composition and structure: “ferro” refers to Fe2+, while “di+molybdenite” indicates the presence of two MoS2 layers.
Unique Identifiers
Mindat ID:
470830
Long-form identifier:
mindat:1:1:470830:4
IMA Classification of Ferrodimolybdenite
Approved
IMA Formula:
Fe2+Mo3+2S2-4
Approval year:
2023
Approval history:
IMA No. 2023-019
Type description reference:
Classification of Ferrodimolybdenite
2.DA.
2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
D : Metal Sulfides, M: S = 3 :4 and 2:3
A : M:S = 3:4
2 : SULFIDES and SULFOSALTS (sulfides, selenides, tellurides; arsenides, antimonides, bismuthides; sulfarsenites, sulfantimonites, sulfbismuthites, etc.)
D : Metal Sulfides, M: S = 3 :4 and 2:3
A : M:S = 3:4
Mineral Symbols
As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Fdmol | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of Ferrodimolybdenite
Metallic
Transparency:
Opaque
Colour:
Grey
Streak:
dark grey
Hardness:
3 on Mohs scale
Tenacity:
Sectile
Cleavage:
Perfect
cleavage in three directions: perfect on {001}, good on {100} and poor on {010}
cleavage in three directions: perfect on {001}, good on {100} and poor on {010}
Fracture:
Conchoidal
Comment:
smooth
Density:
5.445 g/cm3 (Calculated)
Optical Data of Ferrodimolybdenite
Anisotropism:
strong
Reflectivity:
| Wavelength | R1 (%) | R2 (%) |
|---|---|---|
| 400nm | 35.7% | 34.2% |
| 420nm | 35.8% | 34.3% |
| 440nm | 35.9% | 34.3% |
| 460nm | 36.0% | 34.4% |
| 560nm | 36.9% | 35.1% |
| 580nm | 37.1% | 35.7% |
| 589nm | 37.3% | 35.9% |
| 600nm | 37.8% | 36.0% |
Graph shows reflectance levels at different wavelengths (in nm). Peak reflectance is 37.8%.
R1 shown in black, R2 shown in red
Colour in reflected light:
grey to light grey with a bluish tinge
Internal Reflections:
none
Chemistry of Ferrodimolybdenite
Mindat Formula:
FeMo2S4
Element Weights:
Elements listed:
Crystallography of Ferrodimolybdenite
Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
B2/b
Setting:
C2/c
Cell Parameters:
a = 11.8249(8) Å, b = 6.5534(3) Å, c = 13.005(1) Å
β = 114.479(9)°
β = 114.479(9)°
Ratio:
a:b:c = 1.804 : 1 : 1.984
Unit Cell V:
917.21 ų (Calculated from Unit Cell)
Z:
8
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 5.918 Å | (100) |
| 5.194 Å | (42) |
| 2.865 Å | (47) |
| 2.601 Å | (65) |
| 2.597 Å | (33) |
| 2.081 Å | (54) |
| 2.046 Å | (25) |
| 2.037 Å | (57) |
Locality:
Type Occurrence of Ferrodimolybdenite
General Appearance of Type Material:
platy crystals with dimensions ranging from 3×100 µm to 20×40 µm.
Place of Conservation of Type Material:
collections of the Fersman Mineralogical Museum, Russian
Academy of Sciences, Leninskiy Prospekt 18-2, Moscow 115162, Russia, registration number 6005/1
Academy of Sciences, Leninskiy Prospekt 18-2, Moscow 115162, Russia, registration number 6005/1
Geological Setting of Type Material:
was discovered in a differentiated sulfide nodule composed of troilite and pentlandite parts. The nodule was detected in the central zone of a diopside-anorthite-tridymite oval paralava body, approximately 30 metres in diameter, within the pyrometamorphic Hatrurim Complex in Daba-Siwaqa, Jordan.
Associated Minerals at Type Locality:
Other Language Names for Ferrodimolybdenite
Dutch:Ferrodimolybdeniet
German:Ferrodimolybdenit
Related Minerals - Strunz-mindat Grouping
| 2.DA. | Zaykovite | Rh3Se4 |
| 2.DA. | Ezochiite | Cu+(Rh3+Pt4+)S4 |
| 2.DA. | Grimmite | NiCo2S4 |
| 2.DA. | Zolenskyite | FeCr2S4 |
| 2.DA.05 | Shiranuiite | Cu+(Rh3+Rh4+)S4 |
| 2.DA.05 | Fletcherite | CuNi2S4 |
| 2.DA.05 | Florensovite | (Cu,Zn)Cr1.5Sb0.5S4 |
| 2.DA.05 | Siegenite | CoNi2S4 |
| 2.DA.05 | Cadmoindite | CdIn2S4 |
| 2.DA.05 | Kalininite | ZnCr2S4 |
| 2.DA.05 | Violarite | Fe2+Ni3+2S4 |
| 2.DA.05 | Nickeltyrrellite | CuNi2Se4 |
| 2.DA.05 | Linnaeite | Co2+Co3+2S4 |
| 2.DA.05 | Carrollite | CuCo2S4 |
| 2.DA.05 | Cuproiridsite | (Cu,Fe)Ir2S4 |
| 2.DA.05 | Cuprorhodsite | (Cu+0.5Fe3+0.5)Rh3+2S4 |
| 2.DA.05 | Berndlehmannite | Cu(CrV)S4 |
| 2.DA.05 | Polydymite | Ni2+Ni3+2S4 |
| 2.DA.05 | Trüstedtite | Ni3Se4 |
| 2.DA.05 | Daubréelite | Fe2+Cr3+2S4 |
| 2.DA.05 | Cuprokalininite | Cu(Cr3+Cr4+)S4 |
| 2.DA.05 | Greigite | Fe2+Fe3+2S4 |
| 2.DA.05 | Joegoldsteinite | MnCr2S4 |
| 2.DA.05 | Bornhardtite | Co2+Co3+2Se4 |
| 2.DA.05 | Tyrrellite | Cu(Co,Ni)2Se4 |
| 2.DA.05 | Indite | FeIn2S4 |
| 2.DA.05 | Xingzhongite | Pb2+Ir3+2S4 |
| 2.DA.05 | Malanite | Cu+(Ir3+Pt4+)S4 |
| 2.DA.10 | Rhodostannite | Cu+(Fe2+0.5Sn4+1.5)S4 |
| 2.DA.10 | Toyohaite | Ag+(Fe2+0.5Sn4+1.5)S4 |
| 2.DA.15 | Brezinaite | Cr3S4 |
| 2.DA.15 | Heideite | (Fe,Cr)1.15(Ti,Fe)2S4 |
| 2.DA.20 | Konderite | Cu3Pb(Rh,Pt,Ir)8S16 |
| 2.DA.20 | Inaglyite | Cu3Pb(Ir,Pt)8S16 |
| 2.DA.25 | Kingstonite | Rh3S4 |
Other Information
Notes:
The mineral is slightly magnetic
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Internet Links for Ferrodimolybdenite
mindat.org URL:
https://www.mindat.org/min-470830.html
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References for Ferrodimolybdenite
Localities for Ferrodimolybdenite
Showing 1 localities.
Locality List
- This locality has map coordinates listed.
- This locality has estimated coordinates.
ⓘ - Click for references and further information on this occurrence.
? - Indicates mineral may be doubtful at this locality.
- Good crystals or important locality for species.
- World class for species or very significant.
(TL) - Type Locality for a valid mineral species.
(FRL) - First Recorded Locality for everything else (eg varieties).
All localities listed without proper references should be considered as questionable.
Jordan (TL) | |
| Galuskin et al. (2024) +1 other reference |
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