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[R5-10] Minor phases in CI chondrites
Keywords:CI chondrites, Hayabusa 2, Ryugu
Most of the precursor materials of the CI chondrites have been lost during aqueous alteration. Therefore, their properties remain unclear. Revealing the precursors will lead to a better understanding of the Ryugu samples. Here, we report the minor phases in Ivuna and Orgueil that are considered to be the precursors. We identified olivine, spinel, perovskite, hibonite, Os-Ir-Pt alloy, and Fe, Cr-sulfide, indicating that the precursors contain minerals that formed in various environments.