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ordoñezite

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Also known as ordonezite

Ordoñezite or ordóñezite is a rare tetragonal zinc antimonate mineral with chemical formula: ZnSb2O6.

In the Vinony graph

Within Vinony's link graph, ordoñezite is referenced by 4 other articles, and connects out to Mexico, zinc and mineral.

It sits within the topics Antimonate minerals, Minerals described in 1953 and Minerals in space group 136.

Its subject is documented across 5 Wikipedia language editions.

Wikidata facts

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Ordonezite17258-0.jpg
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Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
4.DB.10
chemical formula
ZnSb⁵⁺₂O₆
Nickel-Strunz 9th edition (updated 2009)
4.DB.10
Strunz 8th edition (series ID, updated)
IV/D.04
IMA Mineral Symbol
Ord
Commons category
Ordoñezite
Sources (1)

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Encyclopedic overview

4 sections
Contents
  • Discovery
  • Properties
  • References
  • External links

{{infobox mineral | name= Ordóñezite | image = Ordoñezite natural history museum.JPG | imagesize = | alt = | caption = | category = Antimonate mineral | formula = ZnSb2O6 | IMAsymbol = Ord | molweight = | strunz = 4.DB.10 | dana = | system = Tetragonal | class = Ditetragonal dipyramidal (4/mmm) H-M symbol: (4/m 2/m 2/m) | symmetry = P42/mnm | unit cell = a = 4.66 Å, c = 9.26 Å; Z = 2 | color = Very light to very dark brown, colorless to pearl-gray, light yellowish olive to dark olive | colour = | habit = Pyramidal crystals in drusy or stalactitic masses | twinning = Common on {013} | cleavage = | fracture = Conchoidal | tenacity = | mohs = 6.5 | luster = Adamantine | streak = | diaphaneity = Semitransparent | gravity = 6.635 | density = | polish = | opticalprop = Uniaxial (+) | refractive = N(calculated) = 2.02 - 2.04 | birefringence = | pleochroism = | 2V = | dispersion = | extinction = | length fast/slow = | fluorescence = | absorption = | melt = | fusibility = | diagnostic = | solubility = | impurities = | alteration = | other = | prop1 = | prop1text = | references = }} Ordoñezite or ordóñezite is a rare tetragonal zinc antimonate mineral with chemical formula: ZnSb2O6.

==Discovery== Ordóñezite was first discovered and documented by Ezequiel Ordóñez (1867–1950), a Mexican geologist, formerly director of the Geological Institute of Mexico. It was first described in 1953 for an occurrence with cassiterite in veins in rhyolite in the Santín mine which is located about eight kilometres from Santa Catarina, Guanajuato, Mexico. Another locality is El Antimonio, southwest of Agua Prieta, Sonora, Mexico.

Excerpted from Wikipedia’s “ordoñezite” article, available under the CC BY-SA 4.0 licence.

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