Hapkeite | |
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General | |
Category | Native element minerals |
Formula | Fe2Si |
IMA symbol | Hpk [1] |
Strunz classification | 1.BB.35 |
Crystal system | Isometric |
Crystal class | Hexoctahedral (m3m) H-M symbol: (4/m 3 2/m) |
Space group | Pm3m |
Unit cell | a = 2.831 Å; Z = 1 |
Identification | |
Color | silvery, with a slight tarnish |
Luster | metallic |
Diaphaneity | opaque |
References | [2] [3] [4] |
Hapkeite is a mineral discovered in the Dhofar 280 meteorite found in 2000 in Oman on the Arabian Peninsula. The meteorite is believed to originate from the Moon; specifically, it appears to be a fragment of lunar highland breccia. Hapkeite's composition is of silicon and iron, and it is similar to other silicon-iron minerals found on Earth. An impact on the Moon is thought to have launched the partially molten or vaporized material into orbit.
Due to its 1:2 composition of silicon-iron, hapkeite was given the chemical formula Fe 2 Si. It occurs as opaque, yellowish to silvery microscopic isometric crystals.
It is named after Bruce Hapke, who predicted the presence and importance of vapor-deposited coatings on lunar soil grains (space weathering). [4]
Beside hapkeite, other natural iron silicide minerals include gupeiite, naqite, linzhiite, luobusaite, suessite, xifengite, and zangboite. [3]