随着变形机制、构造环境变化引起成矿流体沸腾作用并导致金矿形成。
With the change of strain dynamic and tectonic situation, ore fluids boil and result the formation of gold deposit.
减压降温导致的流体沸腾作用可能是留村金矿金沉淀成矿的主导因素。
Fluid immiscibility caused by cooling and pressure change was possibly responsible for gold precipitation.
进一步研究发现，矿化与岩浆的结晶分异作用、流体的沸腾作用及流体的混合作用关系密切。
Further studies indicate that mineralization has intimate relationship with magmatic fractional crystallization, fluid boiling and fluid mixing.
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