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The lead-zinc deposit of Fenglishan occurs in the thermal contact metamorphic aureole of intermediate-acid magmatic rocks with marine carbonates of Triassic. 鳳梨山鉛鋅鑛牀産於中酸性巖漿巖與三曡系海相碳酸鹽地層的熱接觸變質(zhì)暈內(nèi)。