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沸腾作用 [fèi téng zuò yòng]
wallop
- 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. - 气液爆破角砾岩体为容矿构造； 成矿作用是在中生代岩浆活动期后气液爆破—沸腾作用下完成的；
Gas—liquid explosive breccia body is the host structure. Mineralization went on under the condition of gas—liquid explosion—boiling action after Mesozoic magmatic activity stage. - 通过包裹体测试的结果分析得出岩浆穹隆的成矿流体属于中高温热液环境，盐度范围比较广，含子晶多相包裹体盐度较高，而富气和富液包裹体的盐度很低，反映了沸腾作用的特征。
It is concluded that ore-forming fluid inside the magma domal structure was formed in the epithermal-mesothermal environment in a relatively wide range of salinity reflecting boiling characteristics .
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