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| Tantalite-(Fe),
formerly known as Ferrotantalite, is named for its dominant
ferrous iron (Fe) content and the Greek mythological
Tantalus (father of Niobe) for the difficulty of dissolving
the mineral.
| Discovered
in 1836;
IMA
status: Valid (pre-IMA; Grandfathered; renamed in 2008) |
|
Chemistry
|
|
|
Chemical
Formula: |
FeTa2O6 |
|
Iron
Tantalum Oxide |
Molecular
Weight: |
513.74 gm |
Composition: |
Tantalum |
70.44 %
|
Ta
|
86.02 %
|
Ta2O5
|
Iron |
10.87 %
|
Fe
|
13.98 %
|
FeO
|
Oxygen |
18.69 % |
O |
|
|
|
100.00 % |
|
100.00 % |
= TOTAL OXIDE |
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Classification
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Mineral
Classification: |
Oxides
|
Strunz 8th
Ed. ID:
|
4/D.18-50
|
Nickel-Strunz 10th
Ed. ID:
|
4.DB.35 |
|
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates) D : Metal: Oxygen = 1:2 and similar B : With medium-sized cations; chains of edge-sharing octahedra
|
Related
to: |
Tantalite-(Fe)-Tantalite-(Mn)
Series. Tantalite-(Fe)-Columbite-(Fe) Series. Dimorphous
with Ferrotapiolite.
|
Synonyms: |
Coltan,
Columbite-Tantalite, Ferrotantalite, Siderotantalite
|
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Crystal
Data
|
|
|
Crystallography:
|
Orthorhombic
- Dipyramidal
|
Crystal
Habit:
|
Commonly
as exsolution intergrowths with ferrotapiolite.
|
Twinning:
|
None
|
|
|
Physical
Properties
|
|
|
Cleavage: |
{100}
Distinct, {010} less Distinct
|
Fracture: |
Irregular/Uneven, Sub-Conchoidal
|
Tenacity:
|
Brittle
|
Moh's
Hardness: |
6.0
- 6.5
|
Density:
|
6.65
- 7.95 (g/cm3)
|
Luminescence:
|
None |
Radioactivity:
|
Not
Radioactive
|
Other: |
Paramagnetic |
|
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Optical
Properties
|
|
|
Color: |
Iron-Black;
Reddish Brown in transmitted light; Gray in reflected
light with Red to Reddish Brown internal reflections
|
Transparency: |
Opaque,
translucent on thin edges
|
Luster: |
Vitreous,
Submetallic
|
Refractive
Index: |
2.260
- 2.430 Biaxial ( - )
|
Birefringence: |
0.170
|
Dispersion: |
Relatively
Strong; r < v
|
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Occurances
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Geological
Setting: |
As
an accessory and primary constituent of granite pegmatites. |
Common
Associations: |
Ferrotapiolite |
Type
Locality: |
Upper Bear Gulch, Tinton pegmatite District, Lawrence Co., South Dakota, USA |
Year
Discovered: |
1836;
IMA changed name from Ferrotantalite to Tantalite-(Fe)
in 2008 |
View
mineral photos: |
Tantalite
Mineral Photos and Locations |
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More
Information
|
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|
|
Mindat.org Webmineral.com
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|
Tantalite-(Fe)
is a fairly rare mineral that is rarely available as
a faceted gem. It is closely related to Tantalite-(Mn),
Columbite-(Fe) and Tapiolite-(Fe). Tantalite and Columbite
are often grouped together as a semi-singular mineral
called Columbite-Tantalite or Coltan. However, Tantalite
has a much greater specific gravity than Columbite (up
to 8.0 for Tantalite compared to Columbite's 5.2). Iron-
rich Tantalite is the mineral Tantalite-(Fe), formerly
known as Ferrotantalite, and manganese-rich Tantalite
is Tantalite-(Mn), formerly known as Manganotantalite.
Tantalite
is also very closely related to Tapiolite. The two minerals
have the same chemical composition, but different crystal
structures; Orthorhombic for Tantalite and Tetragonal
for Tapiolite.
Tantalite
is found as brown to black opaque crystals and Manganotantalite
can be found as brown to red translucent to transparent
crystals and is rarely available as faceted gems that
can be very attractive. Some
Tantalite specimens may show a bluish iridescence and
have weak magnetism.
Material
analyzed by microprobe from: Moss, Norway. At Spittal
an der Drau, Austria. In the Yellowknife district, Northwest
Territories, Canada. At Muhembe, Rwanda. From Nyanga,
Uganda. At Upper Bear Gulch, Lawrence County, South
Dakota, USA.
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