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We also observe chondrules with good ε50Ti and ε54Cr plot with a consistent offset below the primitive chondrule mineral range (PCM), showing that they're from the slope ∼1.0 in the air three-isotope drawing. On the other hand, chondrules with negative ε50Ti and ε54Cr increasingly deviate above from PCM range with increasing δ18O, recommending that they are on a mixing trend with an ordinary chondrite-like isotope reservoir. Additionally, the Δ17O-Mg# systematics of these chondr
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