这表明岩浆起源于受俯冲组分改造或影响的上地幔，且地幔源区存在明显的化学不均一性。
It shows that the magma was derived from the upper mantle which was altered or affected by subduction composition, and the mantle source was of chemical inhomogeneity.
地幔流体ree的研究有助于了解地幔区域化学不均一性、地幔的富集与亏损等地幔地球化学特征。
Study on REE in mantle fluids has significance for understanding of regional geochemical difference, mantle enrichment and depletion.
地幔流体ree的研究有助于了解地幔区域化学不均一性、地幔的富集与亏损等地幔地球化学特征。
Study on REE in mantle fluids has significance for understanding of regional geochemical difference, mantle enrichment and depletion.
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