Oxygen Isotope Fractionation in Perovskite
摘要
） is one of the characteristic accessory minerals in kimberlite and may exceptionally be a major constituent.It is also an accessory mineral in many alkaline intrusives and some metamorphic rocks.Silicates of perovskite structure are very important constituent minerals in the lower mantle of the Earth.In this regard,
引用本文（GB/T 7714）
郑永飞. Oxygen Isotope Fractionation in Perovskite[J]. 中国科学通报：英文版, 1994.
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