不同成矿流体的成矿机制各有差异。
There are some differences in the mineralized mechanisms of different geological fluids.
水—岩交换成矿机制;
吸附作用被认为是低温表生矿床的一种重要的成矿机制。
Adsorption is regarded as an important metallogenic mechanism for the supergene and epithermal ore deposits.
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