Consideridng Rb-Ba-Sr fractionation character and intense deficiency of MREE and using trace element web diagram, the author has revealed the intense magmatic crystallization and differentiation process and pointed out that this process had to do with the compositional variation of biotite and the obvious increase of strontium isotopes.
利用九华山花岗岩体明显的Rb、Ba、Sr变化特征、强烈亏损的中稀土元素特征以及微量元素比值蛛网图和典型的岩石化学变异特征论证了九华山花岗质岩浆的结晶分异作用，探讨了岩浆结晶分异过程对黑云母成分及锶同位素数值的影响，从而指出了岩浆分异作用可能改变I型花岗岩类的黑云母成分标型以及锶同位素初始值的原有特征。
The Abagong iron deposit is attributed to the intrusion and filling of late ore magma by magmatic differentiation and the Mengku, Serblak and Jerbast iron deposits are shared by skarn iron deposits related to the silicic plutons. The shape of ore bodies are controlled by the northwest sub-fault belts near the large regional faults. They are mainly characterized by simple mineral assemblage and skarn alteration for hostrocks.
阿巴宫-蒙库一带铁矿床主要赋存在康布铁堡组中酸性变质火山沉积岩组中，与岩浆活动有关；阿巴宫铁矿属于岩浆分异的晚期矿浆贯入充填型铁矿，蒙库、萨尔布拉克和加尔巴斯套铁矿床是与酸性侵入岩有关的矽卡岩型铁矿；铁矿空间产出位置受深大断裂附近的北西向次级断裂破碎带控制；矿物组合较为简单，围岩蚀变以矽卡岩化为主。
DIGITAL SIMULATION OF VOLATILE EVOLUTION DURING FRACTIONAL CRYSTALLIZATION AND ITS SIGNIFICANCE (2) It contributed to magmatic crystallization differentiation and the concentration of silver in the quartz porphyry magma;
岩浆结晶分异过程中挥发组分演化的计算模拟及其意义②有助于岩浆的结晶分异并导致银在石英斑岩（浆）中的富集；
Massive sulfide deposits and magmatic differentiation
块状硫化物矿床的形成离不开岩浆分异吗？&与姜齐节、秦克章等人商榷
Both root in the unified deep magmatic chamber, belonging to differentiation derivatives at different stages in the deep magmatic chamber. 3.
两者来源于统一的深部岩浆房，属深部岩浆房在不同的阶段分异出的衍生物。
The author regard this kind of ore deposit as magmatic differentiation and segregation ore deposit, not late magmatic ore deposit.
作者认为该类矿床不宜归入晚期岩浆矿床，拟称岩浆分异-分凝矿床。
The existence of local magmatic differentiation, immiscibility and heterogeneity was proved for the pegmatite magmas.
研究表明，伟晶岩存在局部岩浆分异作用，岩浆具不混溶性及非均匀性。
This paper overall deals with the role of controlling ore of volcano-eruptive sedimentary cycle, with respect to the ocurrence, development and evolution of magmatic differentiation, volcanic action, sedimentation and tectonic movement etc.
本文从岩浆分异、火山活动、沉积作用及构造运动等的发生、发展、演化的角度较全面地分析了火山喷发沉积旋回的控矿作用。
These characteristics suggest that the magma originated by partial melting of the lower crust. The rock mass rose and was emplaced rapidiy along fault in a post-orogenic extensional environment, and the magmatic differentiation was incomplete.
地球化学特点表明岩浆由下地壳部分熔融产生；岩体是在造山后伸展构造环境中沿断裂快速上升定位，分异作用不完全状态下形成。