Metamorphosed Calcium-Aluminum-Rich Inclusions in the Tanezrouft 057 CK4 Carbonaceous Chondrite

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Scientific paper

CAIs in TNZ 057, a CK4 chondrite, are abundant (ca. 9.1 area%) and show
evidence of modification by successive nebular and parent body (mainly
metamorphic) processes. These observations confirm the close
relationship between CV and CK chondrites.

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