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EntityQ3976465· pop 10· linked from 5 articles

Suanite is a magnesium borate mineral with formula Mg2B2O5.

Key facts

Mineral.mohs
5.5
Mineral.cleavage
Perfect parallel to {010}
Mineral.name
Suanite
Mineral.category
Borate mineral
Mineral.formula
Mg2B2O5
Mineral.strunz
6.BA.05
Mineral.system
Monoclinic
Mineral.class
Prismatic (2/m) (same H-M symbol)
Mineral.symmetry
P21/a
Mineral.unit cell
a = 12.31 Å, b = 3.12 Å c = 9.2 Å; β = 104.33°
Mineral.color
White to pale gray
Mineral.habit
Clusters of prismatic to fibrous crystals
Mineral.luster
Silky to pearly
Mineral.streak
White
Mineral.diaphaneity
Translucent
Mineral.gravity
2.91
Mineral.opticalprop
Biaxial (–)
Mineral.refractive
nα = 1.596 nβ = 1.639 nγ = 1.670

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Wikidata facts

Image
Suanite.jpg
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Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
6.BA.05
Nickel-Strunz 9th edition (updated 2009)
6.BA.05
Commons category
Suanite
IMA Mineral Symbol
Sua
chemical formula
Mg₂[B₂O₅]
Strunz 8th edition (series ID, updated)
Vc/B.01

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{{Infobox mineral | name = Suanite | image = | alt = | caption = | category = Borate mineral | formula = Mg2B2O5 | molweight = | strunz = 6.BA.05 | dana = | system = Monoclinic | class = Prismatic (2/m) (same H-M symbol) | symmetry = P21/a | unit cell = a = 12.31 Å, b = 3.12 Å c = 9.2 Å; β = 104.33° | color = White to pale gray | habit = Clusters of prismatic to fibrous crystals | twinning = | cleavage = Perfect parallel to {010} | fracture = | tenacity = | mohs = 5.5 | luster = Silky to pearly | streak = White | diaphaneity = Translucent | gravity = 2.91 | density = | polish = | opticalprop = Biaxial (–) | refractive = nα = 1.596 nβ = 1.639 nγ = 1.670 | birefringence = δ = 0.074 | pleochroism = | 2V = 70° | dispersion = | extinction = | length fast/slow = | fluorescence = | absorption = | melt = | fusibility = | diagnostic = | solubility = | impurities = | alteration = | other = | prop1 = | prop1text = | references = }} Suanite is a magnesium borate mineral with formula Mg2B2O5.

It was first described in 1953 by Japanese scientist Takeo Watanabe from the University of Tokyo. His first contact with the mineral was during analysis of gold- and copper- bearing skarn minerals from the Hol Kol mine, located in North Korea obtained in 1939. Due to the small sample size available to him, he was only able to determine the unknown substance's optical properties under a microscope. Watanabe was able to return to the site in 1943 and obtain further samples that permitted him to perform chemical analysis on the material.

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