石英斑岩全岩都发生了矿化，主要矿体产于石英斑岩的中上部。

The whole quartz-porphyry body was mineralized. The main ore body occurs in the upper quartz-porphyry.

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铜(钼)矿(化)体主要产于含矿斑岩体和黑云母花岗斑岩的内外接触带中。

The copper (molybdenum) ore bodies are mainly situated in or out of the contact zone between the mineralized porphyry bodies and the biotite granite porphyry.

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由于这种作用的影响，使钾质煌斑岩的源区地幔处于地温梯度高、氧逸度高的不稳定状态。

Under the influence of the subduction, the source mantle of the potassic lamprophyres has a high geothermal gradient and oxygen fugacity.

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