Numerous fragments totaling 2,106 g were found on 2000 April 14th in the sand desert
of Dar al Gani. Classification and mineralogy: (A. Greshake and M. Kurz):
a fragmental breccia with mineral and lithic clasts set into a ureilitic matrix
dominated by large olivines;
olivine core, Fa14.3-23.5; reduced olivine rims, Fa2.9-13.5;
mineral clasts are pigeonite, Fs14.3Wo8.5 and orthopyroxene, Fs9.3;
lithic clasts consist of fine-grained olivine (Fa22) and pyroxene
(Fs19.3Wo4.5) rich material;
shock stage, S3; low degree of weathering.
type specimen 20.8 g plus one polished thin section MNB
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