拉曼研究表明包裹体矿物具熔融相特征；阴极发光图像中反映出这种锆石具有相对均一的内部结构。
Raman spectrum study indicates that the inclusion minerals show the melting phase feature, and cathodoluminescence images show that this type of zircon has a relatively homogeneous internal structure.
这对高聚物是一完全互溶的共混体系，当共混体系处在熔点和相混合温度之间时，同时存在结晶的熔融相和无定形的相容共混相。
When the temperature of the blend is between melting-point and phase-mixing point, both melting-crystal phase and amorphous miscible phase are present.
后者则分别对应于正交晶相向六方晶相的转变和六方晶相的熔融。
The later corresponded to the transition from orthorhombic phase to hexagonal phase and the melting behavior of hexagonal phase separately.
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