Thus, the phase relations above the solidus of metapelite can be simulated better with the NCKFMASH.Or with other more multiple component systems.
因此,模拟质岩石的固相线以上的相平衡关系最好在NCKFMASH或组分更多的体系进行。
Thus, the phase relations above the solidus of metapelite can be simulated better with the NCKFMASH.Or with other more multiple component systems.
因此,模拟质岩石的固相线以上的相平衡关系最好在NCKFMASH或组分更多的体系进行。
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