
هدانبرژیت
Sign in to saveHedenbergite, CaFeSi2O6 (), is the iron-rich end member of the pyroxene group having a monoclinic crystal system. The mineral is extremely rarely found as a pure substance, and usually has to be synthesized in a lab. It was named in 1819 after M.A. Ludwig Hedenberg, who was the first to define hedenbergite as a mineral. Contact metamorphic rocks high in iron are the primary geologic setting for hedenbergite. This mineral is unique because it can be found in chondrites and skarns (calc–silicate metamorphic rocks). As a member of the pyroxene family, it has generated considerable interest due to
Key facts
- Mineral.name
- Hedenbergite
- Mineral.category
- Inosilicate minerals (single chain)
- Mineral.group
- Pyroxene group, clinopyroxene subgroup
- Mineral.image
- Hedenbergite-Quartz-Hematite-54421.jpg
- Mineral.imagesize
- 260px
- Mineral.formula
- CaFeSi2O6 ()
- Mineral.IMAsymbol
- Hd
- Mineral.molweight
- 248.09 g/mol
- Mineral.strunz
- 9.DA.15
- Mineral.system
- Monoclinic
- Mineral.class
- Prismatic (2/m) (same H-M symbol)
- Mineral.symmetry
- C2/c
- Mineral.color
- Brownish green, black
- Mineral.habit
- Massive, prismatic crystals
- Mineral.cleavage
- Good on {110}
- Mineral.fracture
- Irregular
- Mineral.tenacity
- Brittle
- Mineral.mohs
- 5.5–6.5
via Wikipedia infobox
Wikidata facts
- Subclass of
- mineralogy
- Image
- Mineral Hedemberguita GDFL041.jpg
Show 7 more facts
- Commons category
- Hedenbergite
- Nickel-Strunz 9th edition (updated 2009)
- 9.DA.15
- Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
- 9.DA.15
- solid solution series with
- johannsenite
- crystal system
- monoclinic crystal system
- IMA Mineral Symbol
- Hd
- Strunz 8th edition (series ID, updated)
- VIII/D.01b
Sources (2)
via Wikidata · CC0