SRINIVASAN G. et al. (2001) Ca-K and Al-Mg studies of CIAs
from CH and CR chondrites (MAPS 36-9, 2001, A196, excerpt):

The CAIs from CR chondrites  both with grossite and those with melilite
and hibonite have uniform 26Al abundance suggesting that they formed
within a narrow interval of time from the same reservoir.


Cheers,

Bernd

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