而夕卡岩矿物的逆向分带和富铁夕卡岩矿物的广泛存在则是富铁流体参与夕卡岩成岩作用的结果。
Moreover, the reverse zonation of skarn minerals and widespread occurrence of Fe-rich skarn minerals are the result of Fe-rich fluid participation in the diagenesis and mineralization of skarn.
夕卡岩矿物中硅酸盐熔融包裹体在均一温度和成分方面与含子矿物的流体包裹体和“盐熔”包裹体显著不同。
Silicate melt inclusions are obviously different from daughter minerals bearing fluid inclusions and "salt melt" inclusions in respect of homogenization temperatures and the compositions.
对冬瓜山层控夕卡岩型铜矿床的矿物流体包裹体进行了深入研究。
Comprehensive studies were made for fluid inclusions in minerals of Dongguashan strata-bound skarn deposit.
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