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cliftonite
Cliftonite is a natural form of graphite that occurs as small octahedral inclusions in iron-containing meteorites,〔 such as Campo del Cielo. 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 re-assigned 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.〔
==References==
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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