分离结晶

V-Ti磁铁矿矿床的形成于高Ti玄武岩浆有关，主要受控于岩浆的分离结晶作用；

The V-Ti-magnetite deposits are associated with the high-Ti basaltic magmas and related to fractional crystallization .

CCSD主孔高Ti榴辉岩非耦合的高Ti、低Nb（Zr）特征：对玄武质岩浆房中磁铁矿分离结晶作用的指示

Decoupled high-Ti from low-Nb ( Zr ) of eclogites from the CCSD : Implications for magnetite fractional crystallization in basalt chamber

其次，采用Lyapunov稳定性方法对分离结晶过程进行了稳定性分析。

Secondly , the stability analysis are performed by Lyapunov method .

岩浆分离结晶成因岩浆岩微量元素丰度公式的讨论

Trace element abundances in igneous rocks derived from magma fractional crystallization

判别分离结晶作用和部分熔融作用的一种新方法

A new method of discrimination between fractional crystallization and partial melting

在微重力条件下，大部分分离结晶的过程都是稳定的。

And the detached solidification is most likely stable in the microgravity .

这种分离结晶法可以使得晶体生长的质量得到奇迹般的提高。

This method can improve the quality of crystal dramatically .

成岩作用是分离结晶和同化混染联合作用。

The main diagenesis is fractional crystallization assimilation and contamination .

氨对硝酸钾的选择分离结晶效果较好。

And ammonia had effective selectivity for the separation of potassium nitrate .

多期岩浆分离结晶作用中微量元素丰度关系

Relation between Trace Element Abundances in Multistage Magma Fractional Crystallization in Magma Genesis

地幔平衡部分熔融和岩浆分离结晶成因岩浆岩的判别

Petrogenetic criteria for distinguishing equilibrium partial belting of mantle from magmatic fractional crystallization

用丰度关系法估计岩浆分离结晶过程的物理化学参数

Application of trace elements abundance relationship to estimation of physico-chemical factors in magma fractional crystallization

动态高压下陨石矿物的冲击熔融和分离结晶及其地球化学意义

Shock melting and fractional crystallization of meteorite minerals under dynamic high-pressures and their geochemical significance

岩浆长期分离结晶对岩石锶同位素初始比值的影响

The effect of protracted fractionation of magma on change in initial Sr ratio in granitic batholith

充分的分离结晶作用，是产生这种残余熔浆的主要机制；

Well evolved fractional crystallization is the major mechanism in generation of this kind of residual melts .

用丰度关系法计算分离结晶岩浆岩系总分配系数

Calculation on the general distribution coefficient of the fractional crystallization magma series by the relationship of abundance

金川岩体母岩浆成分及其分离结晶过程的熔浆热力学模拟

Parental Magma Compositions of the Jinchuan Intrusion , Gansu Province and MELTS Thermodynamic Modelling of Fractional Crystallization

源区是软流圈上地幔，玄武岩是部分熔融和分离结晶两种作用的结果。

Two processes of partial melting and fractional crystallization would be responsible for the generation of the basalts .

辉石岩类捕虏体是由该母岩浆高压分离结晶堆积的产物。

The pyroxenite xenoliths could be accumulates of the high - pressure fractional crystallization of the parental magma .

粗面岩的同位素组成和玄武岩接近，说明粗面岩是玄武质岩浆分离结晶作用形成的。

Trachyte has the same isotopic compositions as the basalts , implying that it is generated by fractional crystallization .

高钾岩浆的形成主要受控于批式熔融模式，但也遭受分离结晶作用的影响。

The formation of high-K magma was mainly controlled by batch partial melting , but affected by fractional crystallization .

但在高位岩浆房中，随着分离结晶作用的进行，岩浆的温度和氧逸度逐渐降低。

However , the temperatures and oxygen fugacity of magmas at high level magma chamber decreased along with fractional crystallization .

分离结晶作用和部分熔融作用，是控制玄武岩浆化学成分变异的两种主要方式。

Both fractional crystallization and partial melting are important processes that control the variation of chemical composition of basaltic magma .

水泥地面上滴落状血迹形态的模拟实验地面条件下实现分离结晶的实验研究及数值模拟

An Experimental Study of drip bloodstain on cement ground ; The Experiment on Detached Solidification in Gravity Condition and Numerical Simulation

岩相学及岩石化学研究表明，岩浆演化机制是矿物分离结晶作用。

The petrologic and petrochemical study has shown that the main mechanism controlling the magmatic evolution is fractional crystallization of minerals .

这种反序岩浆演化的机制主要是由于斜长石在高位岩浆房中的分离结晶所致。

The mechanism of this anti-order magmatic evolution is mainly caused by the separate crystallization of plagioclase in a high-level magma chamber .

地幔平衡部分熔融与岩浆分离结晶两种成因模式的微量元素判别式讨论

Discussion on discriminative equations about trace elements of two genetical models of partial fusion of equilibrium in the mantle and magmatic fractional crystallization

玄武质岩浆在演化过程中可能经历了辉石、斜长石、钛铁矿、磷灰石等矿物的分离结晶作用后形成了粗面岩。

Basaltic magma may have experienced the fractional crystallization of pyroxene , plagioclase , ilmenite , apatite and other minerals to form trachyte .

安山质岩浆可由玄武岩岩浆经15%～28%的分离结晶形成。

The andesitic magma could be produced by the fractional crystallization of basalt magma , the fraction of which is 15 to 28 percent .

富钾的火山岩则是原生岩浆在深位岩浆房（>40-50km深度）经镁铁矿物的分离结晶过程演化而来。

The potash-rich volcanic rocks were formed by fractional crystallization of mafic minerals in deep-level chamber ( > 40 ~ 50 km in depth ) .