xanthoxenite
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Xanthoxenite is a rare calcium iron(III) phosphate mineral with formula: Ca4Fe3+2(PO4)4(OH)2·3H2O. It occurs as earthy pale to brownish yellow incrustations and lath shaped crystals. It crystallizes in the triclinic crystal system. It occurs as an alteration product of triphylite in pegmatites. It occurs associated with apatite, whitlockite, childrenite–eosphorite, laueite, strunzite, stewartite, mitridatite, amblygonite and siderite.
Wikidata facts
- Subclass of
- phosphate mineral
- Named after
- compound
Show 8 more facts
- type locality (geology)
- Hennenkobel
- crystal system
- triclinic crystal system
- Nickel-Strunz '10th ed', review of (9th ed/ 2009 update)
- 8.DH.40
- Nickel-Strunz 9th edition (updated 2009)
- 8.DH.40
- streak color
- white
- IMA Mineral Symbol
- Xox
- chemical formula
- Ca₄Fe³⁺₂(PO₄)₄(OH)₂·3H₂O
- Strunz 8th edition (series ID, updated)
- VII/D.15
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Encyclopedic overview
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{{Infobox mineral | name = Xanthoxenite | category = Phosphate minerals | boxbgcolor = | image = | caption = | formula = Ca4Fe3+2(PO4)4(OH)2·3H2O | IMAsymbol = Xox | strunz = 8.DH.40 | system = Triclinic | class = Pinacoidal () (same H-M symbol) | symmetry = P | unit cell = a = 6.7 Å, b = 8.85 Å c = 6.54 Å; α = 92.1° β = 110.1°, γ = 93.2°; Z = 1 | molweight = 739.95 g/mol | color = Pale to brownish yellow | habit = Occurs as platy crystals and as lamellar aggregates and crusts | twinning = | cleavage = Perfect {010} | fracture = | tenacity = | mohs = 2.5 | luster = Earthy (dull) | polish = | refractive = nα = 1.704 nβ = 1.715 nγ = 1.724 | opticalprop = Biaxial (-) | birefringence = | dispersion = | pleochroism = | fluorescence= | absorption = | streak = White | gravity = 2.97 measured, 3.38 calculated | density = | melt = | fusibility = | diagnostic = | solubility = | diaphaneity = Translucent | other = | references = }}
Xanthoxenite is a rare calcium iron(III) phosphate mineral with formula: Ca4Fe3+2(PO4)4(OH)2·3H2O. It occurs as earthy pale to brownish yellow incrustations and lath shaped crystals. It crystallizes in the triclinic crystal system. It occurs as an alteration product of triphylite in pegmatites. It occurs associated with apatite, whitlockite, childrenite–eosphorite, laueite, strunzite, stewartite, mitridatite, amblygonite and siderite.
Excerpted from Wikipedia’s “xanthoxenite” article, available under the CC BY-SA 4.0 licence.