Fig. 17From: Asteroid Ryugu before the Hayabusa2 encounterBackscattered electron image of a portion of a pond deposit clast from the Vigarano CV3 chondrite. The mineralogy of the clast is mainly olivine, with Fe-rich olivine being lighter in shade. Sedimentary beds are apparent, and light gray (Fe-olivine-rich) layers are at the bottoms of the beds. Crossbeds are apparentBack to article page