Sudoite | |
Category: | Chlorite_group |
Formula: | Mg2Al3(Si3Al)O10)(OH)8 |
Color: | White to light green |
System: | Monoclinic |
Mohs: | 2.5–3.5 |
Luster: | pearly, dull |
Refractive: | nα = 1.581 à 1.583 nβ = 1.584 à 1.589 nγ = 1.591 à 1.601 |
Birefringence: | biaxial (-) ; δ = 0.010 to 0.018 2V = 64 to 70° (measured) 2V = 68 to 72° (calculated) |
References: | .[1] [2] |
Sudoite is a mineral from the chlorite group. It was named after Toshio Sudo (1911-2000), professor of mineralogy at the University of Tokyo, in Japan, and a pioneer of clay science.[3] The mineral tosudite also wears his name. It was approved as a valid species by the International Mineralogical Association in 1966.
Sudoite is a clay mineral with chemical formula defined as Mg2Al3(Si3Al)O10)(OH)8. it has a monoclinic crystal system. Its hardness on the Mohs scale is comprised between 2.5 and 3.5.
Following the Nickel–Strunz classification, it is contained in the "09.EC.55" group:
scope=col | Mineral | scope=col | Formula | scope=col | Symmetry group | scope=col | Space group |
---|---|---|---|---|---|---|---|
1 or | C1 or C | ||||||
(x ≤ 0,33) | 2/m | C2/m | |||||
2/m | C2/m | ||||||
2/m | C2/m | ||||||
, 2 or 2/m | C, C2 or Cc | ||||||
2/m | C2/m | ||||||
2 | C2 | ||||||
1 | C1 | ||||||
unknown | |||||||
2/m | C2/m | ||||||
m | Cm | ||||||
unknown | |||||||
2/m | C2/m | ||||||
Sudoite | 2/m | C2/m |
It has been first discovered in the Knollenberg Keuper formation, in the village of Plochingen, Stuttgart Region (Baden-Württemberg, Germany).[4] Despite being an unlikely mineral, it has been described in every continent but Antarctica and Oceania. It is found mainly in hydrothermal or high-pressure/low-temperature (HP/LT) metamorphism contexts[5] [6] [7]
This mineral has been used as gemstone for the production of personal ornaments, beads and pendants, during the Early Ceramic Age (500 BC – 500 AD), in the Lesser Antilles.[8] The precise source of such formation of sudoite allowing to carve artifacts in rather large blocks remain unknown.
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