In the Yanzhuang H6 meteorite are small (10 mu m to 7mm) Fe-Ni dendrit
es in pockets and veins. We have characterized the surface morphology
of several of the dendrites by using scanning electron microscopy (wit
h X-ray microanalysis). The dendrite surface has a network of growth l
edges. At the edge of the apexes of the dendrites, there are four conc
entric ''rings'' which are consistent with a [111] dendrite growth dir
ection to produce four ring patterns parallel to the {100} planes. The
Fe dendrites are partially coated with a material containing growth l
edges which is rich in Fe and S, and is presumed to be FeS (troilite).