NWA 13784 CV3-an was brought to us by Hanno Strufe and Andreas Grünemeyer, described by Ansgar Greshake with oxygen isotopes by Karen Ziegler.
It appears to have been affected by both water and shock. Olivine grains are strongly zoned from their centers out. Undulatory extinction is evident in some chondrules. A set of subparallel fractures separate offset blocks. Multilayered chondrules are common. Opaque phases are said to be troilite and taenite.