melt inclusion meaning in Chinese
熔融体包裹体
Examples
- The methods for observing melt inclusion on grinded sample slice and the identification marks of entirely uncovered melt inclusion are also introduced in this paper
文中还介绍了样品磨毛后观察其中包裹体的方法以及包裹体完全磨出表面后的若干识别标志。 - The compositions of usual elements and rare earth elements and inclusions of corundum megacrysts related to alkali basalt in changle , shandong province , are analyzed . in the main parts of corundum megacrysts are a large number of fluid - melting inclusions , zircon , ta - columbite inclusions , and in the central crystal core are a large number of melting inclusions . the corundum megacrysts were formed in different periods and different physical chemistry conditions . the crystal core was formed in magma system , and the main parts were formed in inhomogeneously geochemical conditions in which magam and fluid phases coexisted
分析山东昌乐与碱性玄武岩有关的刚玉巨晶不同部位的常量元素、稀土元素及包裹体组成.刚玉巨晶的主体以大量流体?熔体包裹体、锆石、铌(钽)铁矿包裹体为主，而巨晶中的“晶核”部位则以大量的熔体包裹体为主，反映研究区的刚玉巨晶是在不同的阶段形成的.刚玉“晶核”以及“铜皮刚玉”形成于熔体相为主的体系中，而主体刚玉则形成于熔体?流体过渡的急剧变化的不均一的地球化学环境中 - In view of smaller and thinner samples required in grinding slice for microprobe analysis , three steps are used : establishing a thinner grinding plane on the center of homogenized crystalloid melt inclusion sample , grinding the surrounding parts of the sample to the thickness as the center , polishing the grinded sample slice in order to expose the melt inclusion to the sample surface
摘要针对磨制样品十分细小和较薄等特点，采用如下三个步骤磨制：以加热过的细小样品为中心创建一磨制平面；将样品周围的岩石薄块磨至接近细小样品的相同厚度；在抛光机上抛光，使包裹体完全露出表现。 - Sapphire from shandon and hainan commonly have the reaction border , we found out this reaction border enriched with fe , mg , and k by testing its components ; we also studied the inclusion in the sapphire , and found many kc1 crystal grain with variety of size , a melt inclusion enriched with k , si , is also found , this may suggest an assimilationary - magmatic course ; besides that , another minerl inclusions such as enstenite , magnetite , chromite , zircon are also found
3 、观察到了山东、海南蓝宝石普遍存在的反应边，并测试了反应边的成分，证实其以富fe ， mg ，和k为特征；研究了蓝宝石里面的包体，发现蓝宝石里面存在着大小不等的kcl的结晶颗粒，还发现了富k富si的熔浆包裹体，说明其形成过程中有同化混染的贡献；此外还发现了斜方辉石，磁铁矿，铬铁矿，锆石的包体矿物。