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The abundance and distribution of selected minor and trace elements (Ti. Zr, Y, Nb, Ce, Ga and so) in fresh volcanic rocks cam be used to clses / fy the differentiation products of subalkaline and alkaline magma series in a ndmflsr manner to methods using normative or major-element indices. As these elements are immobile during po0t-cousidation alteration and metamorphic processes,
- Author
- Ari Rangel
- Language
- EN