Classification: Chondrite L-melt breccia S4/W1
Place/Time: 01.2015 in Zagora, Morocco
Petrography: The meteorite is composed of regions displaying chondritic textures with recognizable chondrules intermingled with abundant melt regions characterized by recrystallized shock melt and characteristic FeNi metal and sulfide globules. Olivine and pyroxene show strong mosaicism attesting to a high degree of shock metamorphism.
Both side super mirror polished. Higher preparation quality.