Skip to content
EntityQ424367· pop 17· linked from 77 articles

Tephroite is the manganese endmember of the olivine group of nesosilicate minerals with the formula Mn2SiO4. A solid solution series exists between tephroite and its analogues, the group endmembers fayalite and forsterite. Divalent iron or magnesium may readily replace manganese in the olivine crystal structure.

Key facts

Mineral.name
Tephroite
Mineral.category
Silicate mineral
Mineral.image
Tephroite Manganese silicate Kaao Mine Tochigi-ken Honshu Japan 1816.jpg
Mineral.caption
Tephroite from Japan
Mineral.formula
Mn2SiO4
Mineral.IMAsymbol
Tep
Mineral.system
Orthorhombic
Mineral.class
Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m)
Mineral.symmetry
Pnma (no. 62)
Mineral.unit cell
a = 4.88(2) Å, b = 10.61(2) Å c = 6.24(2) Å; Z = 4
Mineral.color
Olive-green, bluish green, gray, °esh-red, reddish brown; pale green in thin section, may be colorless
Mineral.habit
Crystals typically short, prismatic, to 4 cm, or anhedral, equidimensional. Commonly in disseminated grains, compact, or massive.
Mineral.twinning
Uncommon on {011}
Mineral.cleavage
{010}, distinct; {001}, imperfect
Mineral.fracture
Uneven to conchoidal
Mineral.tenacity
Brittle
Mineral.mohs
6
Mineral.luster
Vitreous to greasy

via Wikipedia infobox

Wikidata facts

Image
Tephroite and Willemite - Franklin Mine, Sussex County, New Jersey, USA.jpg
Show 7 more facts
IMA Mineral Symbol
Tep
Strunz 8th edition (series ID, updated)
VIII/A.03
Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
9.AC.05
Commons category
Tephroite
Nickel-Strunz 9th edition (updated 2009)
9.AC.05
chemical formula
Mn²⁺₂SiO₄
Mohs' hardness
6
Sources (2)

via Wikidata · CC0

~3 min read

Article

1 sections
Contents
  • References

{{infobox mineral | name = Tephroite | category = Silicate mineral | boxwidth = | boxbgcolor = | image = Tephroite Manganese silicate Kaao Mine Tochigi-ken Honshu Japan 1816.jpg | imagesize = | alt = | caption = Tephroite from Japan | formula = Mn2SiO4 | IMAsymbol = Tep | molweight = | strunz = | dana = | system = Orthorhombic | class = Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) | symmetry = Pnma (no. 62) | unit cell = a = 4.88(2) Å, b = 10.61(2) Å c = 6.24(2) Å; Z = 4 | color = Olive-green, bluish green, gray, °esh-red, reddish brown; pale green in thin section, may be colorless | colour = | habit = Crystals typically short, prismatic, to 4 cm, or anhedral, equidimensional. Commonly in disseminated grains, compact, or massive. | twinning = Uncommon on {011} | cleavage = {010}, distinct; {001}, imperfect | fracture = Uneven to conchoidal | tenacity = Brittle | mohs = 6 | luster = Vitreous to greasy | streak = Pale gray | diaphaneity = Transparent to translucent | gravity = 3.87 – 4.12 | density = | polish = | opticalprop = Biaxial (−) | refractive = nα = 1.759 nβ = 1.797 nγ = 1.860 | birefringence = δ = 0.101 | pleochroism = Weak; X = brownish red; Y = reddish; Z = greenish blue. | 2V = Measured: 60° to 70°, Calculated: 78° | dispersion = | extinction = | length fast/slow = | fluorescence= | absorption = | melt = | fusibility = | diagnostic = | solubility = | other = | alteration = | references = }} Tephroite is the manganese endmember of the olivine group of nesosilicate minerals with the formula Mn2SiO4. A solid solution series exists between tephroite and its analogues, the group endmembers fayalite and forsterite. Divalent iron or magnesium may readily replace manganese in the olivine crystal structure.

It was first described for an occurrence at the Sterling Hill Mine and Franklin, New Jersey, United States. It occurs in iron-manganese ore deposits and their related skarns. It also occurs in metamorphosed manganese-rich sediments. It occurs in association with: zincite, willemite, franklinite, rhodonite, jacobsite, diopside, gageite, bustamite, manganocalcite, glaucochroite, calcite, banalsite and alleghanyite. It can also be found in England and Sweden.

Connections

Categories