Physics
Scientist
Elemental and isotopic fractionations produced through evaporation of the Allende CV chondrite: Implications for the origin of HAL-type hibonite inclusions
Isotopic and Elemental Fractionations Produced During Evaporation of the Allende Carbonaceous Chondrite
Trace Element Fractionations in Hibonite-bearing Evaporation Residues: Comparison with HAL-type Hibonite Inclusions
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