Abstract
Cover: Background–Orion Nebula; bottom left corner–combined elemental map in Mg (red), Ca (green), and Al Kα X–rays of a compound ultrarefractory CAI–bearing inclusion from the reduced CV3 carbonaceous chondrite Efremovka. The CAI consists of a Fluffy Type A inclusion, an ultrarefractory inclusion, and an amoeboid olivine aggregate (see paper by Ivanova et al. on p. 2107).
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