May 28 2014
Carlfriesite was first discovered in 1975 from the Oriental (Bambollita) mine, north-east of the Moctezuma (Bambolla) mine, 12km south of Moctezuma, Sonora, Mexico.
It was named after Carl Fries, Jr. (1910-1965), U.S. Geological Survey and the Geological Institute of the National University, Mexico City, Mexico.
Properties of Carlfriesite
The following are the key properties of Carlfriesite:
- Cell Data
- Space Group: C2/c
- a = 12.576(2)
- b = 5.662(3)
- c = 9.994(2)
- β = 115.56(3)°
- Z = 4
- Crystal Data
- Monoclinic
- Point Group: 2/m
- As euhedral prismatic crystals, to 5mm, with an “axe head” appearance due to {010} and other forms being curved, in radial sprays;typically in botryoidal crusts
- X-ray Powder Pattern: 3.167 (10), 3.082 (9b), 5.063 (6), 2.832 (6), 3.369 (4), 4.825 (3), 2.698 (3)
- Chemical Composition
Elements |
Content 1 |
Content 2 |
Content 3 |
TeO2 |
87 |
89.5 |
57.94 |
CaO |
10.2 |
10.5 |
10.18 |
H2O |
6.5 |
- |
- |
TeO3 |
- |
- |
31.88 |
Total |
103.7 |
100 |
100 |
- Optical Properties
- Optical Class: Biaxial (–)
- Pleochroism: Weak; in yellow
- Orientation: Y = b; X ^ c = 28°.
- Absorption: X = Y < Z
- α = 1.982
- β = 2.095
- γ = 2.19
- 2V(meas.) = 80°
- 2V(calc.) = 79°
- Estimated Properties
Electron density |
Bulk density (electron density) = 4.97 g/cm3
note: Specific gravity of Carlfriesite = 5.7 g/cm3 |
Photoelectric |
PECarlfriesite = 245.73 barns/electron
U= PECarlfriesite x ρ Electron density = 1220.46 barns/cm3 |
Fermion index |
Fermion index = 0.05
Boson index = 0.95 |
Radioactivity
|
Carlfriesite is not radioactive
|
How to Identify Carlfriesite
Carlfriesite is a yellow mineral with distinct cleavage and yellow streak.
The density of the mineral is 6.3 g/cm3, and its hardness is 3.5.
Global Distribution
Carlfriesite is widely distributed in the Oriental (Bambollita) mine, north-east of the Moctezuma (Bambolla) mine, 12km south of Moctezuma, Sonora in Mexico.
Occurrence of Carlfriesite and Useful Mineral Association
Carlfriesite occurs in cavities in an oxidized hydrothermal Au–Te deposit in intensely silicified brecciated rhyolite vitrophyre.
It is closely associated with hessite, galena, bornite, barite, dickite, calcite, cesbronite, argentian gold, chlorargyrite, and cerussite.
References