Oxygen isotopic compositions of aluminum-rich chondrules
from CH chondrites. Five out of eight chondrules analyzed exhibit large internal-isotopic heterogeneity, whereas others are isotopically uniform; all chondrules have porphyritic minerals. In contrast to aluminum-rich chondrules in ordinary
chondrites, oxygen isotopic heterogeneity is due to the presence
of relict CAIs. These relict CAIs are chondrules, being composed of hibonite, grossite, melilite, perovskite, and platinum group metals.