immiscibility

基本解釋

The three phase immiscibility of Fanshan magma resulted in the formation of three phosphorus ore zones.
礬山巖漿的三相不混溶作用導致了礬山三個礦帶的形成。
This implies that the liquid immiscibility in felsic magma can directly induce the formation of porphery deposit.
這意味著長英質巖漿中的液態(tài)不混溶可直接導致斑巖礦床的形成。
However,the immiscibility of oil with methanol leads to low transesterification rate in the biodiesel production.
但在傳統(tǒng)的生物柴油生產工藝中,由于原料油與醇的不互溶性,嚴重影響了酯交換反應的程度。
Furthermore, the immiscibility can enrich rare elements to high level, which owe to the affinity of volatile like F, B, P, etc to rare elements.
還對稀有金屬有高度富集作用，這主要歸功于F、B、P等揮發(fā)份對稀有金屬元素的親和力。
Fluid immiscibility, continuous influxing of meteoric water and water-rock exchange are very important factors that caused gold and stibnite to deposit.
流體不混溶、大氣降水的不斷加入以及水-巖交換作用是導致本區(qū)成礦流體中金、銻淀積成礦的主要因素。