混溶，就是几种物质混在一起，能相互融合的现象。
梵山富含磷的岩浆经历了解体，因此产生了三种不混溶的液体：高岭土岩浆，叠合岩浆和磷酸盐熔体。
The Fanshan phosphorus-rich magma experienced unmixing and hence produced three sorts of immiscible liquids:pyroxenitic magma, syenitic magma and phosphate melt.
矾山岩浆的三相不混溶作用导致了矾山三个矿带的形成。
The three phase immiscibility of Fanshan magma resulted in the formation of three phosphorus ore zones.
其余1%的钙存在于软组织，细胞外液及血液中，称之为混溶钙池。
And 1% in parenchyma, extracellular fluid and blood, called the Immiscibility calcium pool.
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