Aspects of this topic are discussed in the following places at Britannica.
In meteorites, the olivine is usually a forsteritic variety containing only Fa15 to Fa30. In the Nakhla (Egypt) meteorite (an achondrite meteorite), the olivine is more ferrous, however, containing as much as Fa65. In the chondrites (stony meteorites), the olivine is commonly incorporated in the distinctive spheroidal bodies...
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