Chondrule-Cored Aggregates in CV Chondrites: Origin by Chondrule Formation Followed by Olivine Condensation

Fagan T. J. Yasuda T. Nagashima K. Krot A. N.

80th Annual Meeting of the Meteoritical Society 2017 [#6202]


“Chondrule-cored aggregates (ChCAs) are a new component of CV chondrites, in which early-stage pyroxene crystallized from chondrule melt and was followed by olivine condensation. We describe two ChCAs from Allende and a related object in Vigarano.