NWA 6368 					Location Unknown

(before was offered as paired to NWA 3118) 						
Morocco  

Purchased: Apr 2009 

Carbonaseous Chondrite CV3 

Petrography: (M.A. Ivanova, Vernad.) The meteorite consists of fine-grained matrix material, chondrules and their fragments, 
refractory inclusions (CAIs) and isolated grains of minerals. Large CAIs (up to 2 cm) are abundant in this meteorite, 
the main assemblage of their minerals: spinel, melilite, pyroxene, anorthite and hibonite. The main minerals of the meteorite are olivine and pyroxene. 
The minor phases are plagioclase, spinel, chromite, sulfides, and Fe,Ni metal grains.

Geochemistry: Mineral compositions and geochemistry: Olivine (EMP) is Fa1-21. Pyroxene is represented by low-Ca pyroxene Fs1-13Wo0.5-5En86-98, 
and augite Fs2-11Wo28-33En60-65.