09030 - Partial Complete NWA Unclassified Ordinary Chondrite Meteorite 5.6 g With Fusion Crust Peipiaosteus pani During the lower Cretaceous

During the lower Cretaceous

This specimen has a cluster of many lustrous and well defined crystals

Petrography: Slices from several stones show similar metal/olivine ratio

and surprisingly

and/or fused soil

09030 - Partial Complete NWA Unclassified Ordinary Chondrite Meteorite 5.6 g With Fusion Crust Peipiaosteus pani During the lower CretaceousThese meteorites were found in the Saharan Desert in Northwest Africa, likely by nomads. In order to classify them it would be necessary to cut off a section for analysis. Although they are exceedingly rare when compared to terrestrial rocks, these are the most abundant type of meteorite and are referred to as common chondrites. H and L (designating the amount of metal contained) type chondrites have been already extensively studied. Composed largely