It occurs associated with kamacite, taenite, schreibersite, cohenite, pentlandite and magnetite.
3.
On Earth cohenite is stable only in rocks which formed in a strongly B�hl near Kassel in Germany.
4.
An iron nickel phosphide, schreibersite, is present in most nickel-iron meteorites, as well as an iron-nickel-cobalt carbide, cohenite.
5.
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.
6.
"' Cohenite "'is a naturally occurring iron carbide mineral with the chemical structure ( C . This forms a hard, shiny, silver mineral which was named by E . Weinschenk in 1889 after the German mineralogist Emil Cohen, who first described and analysed material from the Magura meteorite found near Slanica, } ilina Region, Slovakia.
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