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Martian Meteorites | Lunar Rocks | HED Group | PAC Group | Carbonaceous Chondrites | Rare Chondrites Last Updated: 17 January 2018


The ureilites are named for Novo Urei, a rural village in the Mordova Republic, Russia, where several meteorites fell in late 1886. 

The ureilites are subdivided into two groups: the monomict main group and the less common polymict group. Main group ureilites are composed largely of coarse-grained olivine and minor pyroxene, mostly in the form of calcium-poor pigeonite, set in a dark carbonaceous matrix of graphite and diamond, nickel-iron metal, and troilite. Our recent find, El Gouanem, Morocco, is a rather typical member of the main group. Polymict ureilites consist of a mixture of different lithologies. Besides clasts from main group ureilites, they contain magmatic inclusions, dark carbonaceous clasts, chondritic fragments of different origins, and various other inclusions. This suggests a surface or regolith origin for the polymict ureilites, an assumption that is supported by the values for noble gases that have been implanted into the regolith by the solar wind.


DAG 319

Polymict Ureilite DAG 319

Lybia, found in 97

TKW : 740 gr


DAG319 -00

5.89 gr

superb slice with large dark inclusions


DAG319 -01

3.15 gr

non parallel slice with crust


DAG319 -02

6.17 gr

end cut covered with deep black crust


DAG319 -03

11.57 gr

end cut with free iron blobs and several dark inclusions


DAG319 -04

12.12 gr

end cut with deep black crust and several dark inclusions !


DAG319 -05

3.48 gr

end cut with deep black crust and several dark inclusions !




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