The Xifanping porphyry copper deposit is located in the southwestern Sichuan Province.

四川盐源西范坪斑岩铜矿床中存在大量钾长环斑结构.

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Therefore, the illite polytype might be an effective indictor for mineralization of porphyry copper deposit.

在此, 斑岩铜矿中伊利石多型可能成为有效的矿化晕指示剂.

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The geochemical and geological characteristics are the same a those of a porphyry copper deposit.

矿床地球化学特征、矿体特征均显示出斑岩型铜矿床特点.

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