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X-ray mapping is increasingly used in the geological sciences for qualitative observations of textures, mineral zoning, and element distribution among rock components     . We combine mapping with an aggressive program of image analysis in deepening our understanding of the early solar system through the analysis of chondritic meteorites [5, 6] . Chondrites are "sediments" that accreted in the earliest solar system into planetesimals now represented by objects in the asteroid belt.doi:10.1017/s1431927614005480 fatcat:kvhzgncbt5gshinsvvyoz4pfs4