porphyry copper-silver-tin deposit
porphyry copper-silver-tin deposit
斑岩型铜银锡矿床
以上为机器翻译结果，长、整句建议使用 人工翻译 。
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It is a porphyry copper-silver-tin deposit that occurs in the transitional crust and was formed by derivatives of the lower crustal-upper mantle transitional magma.
它是分布于过渡性地壳上的、由起源于下地壳—上地幔的过渡性岩浆的衍生物形成的斑岩型铜银锡矿床。
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