Fig 8.jpg
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Fig. 8. Variation of δ30Si vs. CI chondrite-normalized K/Ca (a) non-porphyritic chondrule silicates and in (b) porphyritic chondrule silicates of this study. Non-systematic variations of δ30Si and K/Ca in chondrule phases may reflect differences in the volatilities of K, Ca and Si, and the different partitioning of these elements between olivine, pyroxenes and mesostasis.
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创建时间：
2023-10-27
