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| Durangite
is named for the original occurrence in Durango, Mexico.
| Discovered
in 1869;
IMA
status:
Valid (pre-IMA; Grandfathered) |
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Chemistry
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Chemical
Formula: |
NaAl(AsO4)F
|
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Sodium
Aluminum Arsenate Fluoride |
Molecular
Weight: |
207.89 gm
|
Composition: |
Sodium |
11.06 % |
Na |
14.91 % |
Na2O |
|
Aluminum |
12.98 % |
Al |
24.52 % |
Al2O3 |
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Arsenic |
36.04 % |
As |
55.28 % |
As2O5 |
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Oxygen |
30.78 % |
O |
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Fluorine |
9.14 % |
F |
9.14 % |
F |
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|
— % |
F |
-3.85 % |
-O=F2 |
|
|
100.00 % |
|
100.00 % |
= TOTAL OXIDE |
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Classification
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Mineral
Classification: |
Arsenates
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Strunz 8th
Ed. ID:
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7/B.25-50
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Nickel-Strunz 10th
Ed. ID:
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8.BH.10
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8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
H : With medium-sized and large cations, (OH,etc.):RO4 = 1:1
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Related
to: |
Tilasite Group.
Forms two series; Durangite-Maxwellite Series
and Durangite-Tilasite Series. Isostructural with Titanite.
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Members
of Group: |
Tilasite Group:
Isokite, Lacroixite, Maxwellite, Panasqueiraite, Tilasite.
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Varieties: |
None
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Synonyms: |
ICSD 30205,
PDF 36-424
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Crystal
Data
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Crystallography:
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Monoclinic
- Prismatic
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Crystal
Habit:
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Typically in euhedral oblique
pyramidal crystals, to 1 cm, slightly elongated along [001], with dominant
{110}, {111}, and {010}, {100}, {021}, faces commonly dull
and rough; in stacked aggregates. Artificial crystals are prismatic [101], and rarely tabular.
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Twinning:
|
On {001} common as interopenetration twins (artificial crystals).
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Physical
Properties
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Cleavage: |
Distinct
on [110]
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Fracture: |
Irregular/Uneven
to Conchoidal
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Tenacity:
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Brittle
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Moh's
Hardness: |
5.0
- 5.5
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Density:
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3.90
- 4.07 (g/cm3);
Density is highest in dark-coloured, ferrian material.
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Luminescence:
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None
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Radioactivity:
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Not
Radioactive
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Optical
Properties
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Color: |
Pale to dark red-orange, deep red, orange,
orange-brown, pale yellow; in transmitted light, color zoned from varying contents of Fe and Mn.
Green color exhibited by artificial material.
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Transparency: |
Transparent
to Opaque |
Luster: |
Vitreous,
usually dull |
Refractive
Index: |
1.634
- 1.685
Biaxial ( - )
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Birefringence: |
0.051
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Dispersion: |
Strong, also weak to moderate; r <
v, less commonly r > v |
Pleochroism: |
X
= yellow-orange; Y
= pale yellow-orange; Z
= nearly colorless. |
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Occurances
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Geological
Setting: |
In veins in alkalic rhyolite and tin placers derived therefrom; in pegmatite dikes in
granite. |
Common
Associations: |
Cassiterite, Hematite, Topaz, Ilmenite, Tantalite, Wickmanite, Beudantite, Mimetite,
Fluorite, Tridymite, Cristobalite, Quartz, Amblygonite, “Chalcedony”, Zeolites, clay minerals.
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Common
Impurities: |
None
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Type
Locality: |
Barranca Mine, Coneto de Comonfort, Mun. de Coneto de Comonfort, Durango, Mexico
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Year
Discovered: |
1869
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View
mineral photos: |
Durangite
Mineral Photos and Locations |
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More
Information
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|
Mindat.org
Webmineral.com
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Durangite
is named for the type locality at the Barranca mine in the
Durango state of Mexico. Durangite occurs in veins of alkalic
rhyolite and tin placers that were derived from alkalic rhyolites and in
pegmatite dikes through granite. Durangite is an extremely rare gem. Durangite crystals
are found in colors of pale to dark red-orange, deep red, orange,
orange-brown and pale yellow. The two most notable occurances
for possible gem quality crystals are the Barranca tin mine, about 30 km northeast of Coneto de Comonfort,
Durango, Mexico and in the Thomas Range, Juab County, Utah.
Other
Durangite locations are near Lake Ramsey, New Ross, Nova Scotia, Canada;
in tin prospects near Boiler Peak, in the Black Range, Sierra County, New Mexico,
USA; at the Cheesewring quarry, Linkinhorne, Cornwall, England.
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Durangite
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