Heavily-Metamorphosed Clasts in the CV Carbonaceous Chondrite Mokoia: Evidence for Strong Thermal Metamorphism on the CV Parent Asteroid

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Scientific paper

The mineralogy and O-isotope compositions of heavily-metamorphosed
clasts from the Mokoia CV breccia are consistent with those of CV
chondrites, suggesting an origin of the clasts in the interior of the CV
parent asteroid.

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