Cliftonite (original) (raw)

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dbo:abstract Cliftonite is a natural form of graphite that occurs as small octahedral inclusions in iron-containing meteorites. It typically accompanies kamacite, and more rarely schreibersite, cohenite or plessite. Cliftonite was first considered to be a new form of carbon, then a pseudomorph of graphite after diamond, and finally reassigned to a pseudomorph of graphite after kamacite. Cliftonite is typically observed in minerals that experienced high pressures. It can also be synthesized by annealing an Fe-Ni-C alloy at ambient pressure for several hundred hours. The annealing is carried out in two stages: first a mixture of cohenite and kamacite is formed in air at ca. 950 °C; it is then partly converted to cliftonite in vacuum at ca. 550 °C. The Campo del Cielo region of Argentina is noted for a crater field containing a group of distinctive iron meteorites. (en)
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dbp:category dbr:Mineral
dbp:class dbr:H-M_symbol Dihexagonal dipyramidal (en)
dbp:color Gray (en)
dbp:formula dbr:Carbon
dbp:habit Octahedra, cubes, cubo-octahedra, cubo-dodecahedra; isolated or aggregated, ca. 20 μm in size (en)
dbp:luster Sub-metallic (en)
dbp:mohs 1 (xsd:integer)
dbp:name Cliftonite (en)
dbp:streak gray (en)
dbp:symmetry P63/mmc (en)
dbp:system dbr:Hexagonal_crystal_system
dbp:wikiPageUsesTemplate dbt:Reflist dbt:Infobox_mineral
dcterms:subject dbc:Allotropes_of_carbon dbc:Native_element_minerals dbc:Hexagonal_minerals dbc:Minerals_in_space_group_194
gold:hypernym dbr:Form
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rdfs:comment Cliftonite is a natural form of graphite that occurs as small octahedral inclusions in iron-containing meteorites. It typically accompanies kamacite, and more rarely schreibersite, cohenite or plessite. The Campo del Cielo region of Argentina is noted for a crater field containing a group of distinctive iron meteorites. (en)
rdfs:label Cliftonite (en)
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prov:wasDerivedFrom wikipedia-en:Cliftonite?oldid=1072372445&ns=0
foaf:isPrimaryTopicOf wikipedia-en:Cliftonite
foaf:name Cliftonite (en)
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