The microscopic observation and homogenization temperature determination experiment of melt inclusions in plagioclase and olivine in basalt phenocrysts from the Mariana Trough were made.
对马里·亚纳海槽玄武岩斜长石和橄榄石斑晶中的熔融包裹体进行了镜下观察和均一化测温实验。
Silicate melt inclusions are obviously different from daughter minerals bearing fluid inclusions and "salt melt" inclusions in respect of homogenization temperatures and the compositions.
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。
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