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The Mineralia Collection
Transitional Pallasite Meteorite
Olivine (peridot) crystals in an iron-nickel matrix. Coarser metal areas develop Widmanstätten patterns upon etching. Theorized as formed of core-mantle boundary material of early differentiated bodies fragmented by collision.
Type: Stony-iron, Coarse octahedrite
Group: Main Group Pallasite
Magadan Oblast, Russia