- Source: Diiron silicide
- Kamus rumus kimia
- Diiron silicide
- Iron silicide
- Dicobalt silicide
- List of minerals recognized by the International Mineralogical Association (H)
- List of minerals recognized by the International Mineralogical Association (P–Q)
- List of minerals recognized by the International Mineralogical Association (L)
- List of minerals recognized by the International Mineralogical Association (S)
- List of minerals recognized by the International Mineralogical Association (C)
- List of minerals recognized by the International Mineralogical Association (M)
- List of minerals recognized by the International Mineralogical Association (W–X)
Diiron silicide (Fe2Si) is an intermetallic compound, a silicide of iron. It occurs in cosmic dust as the mineral hapkeite. It is a non-stoichiometric compound where the Fe:Si ratio depends on the sample preparation. A related compound Fe5Si3 occurs in nature as the mineral xifengite.
See also
Ferrosilicon