Trace Element Abundance Relationships in the Multi-stage Comagmatic Fractional Crystallization and Their Applications

In this study a mathematical expression of trace element abundance relationship for the mul-ti-stage comagmatic fractional crystallization has been established ,based on geochemical studies of the Emeishan basalt-trachyte series and adjacent mafic-ultramafic layered intrusions, as well as on the avail-able data for basalt, andesite, dacite and rhyolite series in southern Andes,Chile ,which have been well documented.It is demonstrated that the abundance constant (R) for a given trace element at dif-ferent stages of fractional crystallization of a parental magma is highly variable,which can be used as a criterion to divide fractional crystallization stages.

Estimation of the Primary Magma Compositions of an Igneous Rock Series Petrogenetically Associated with Fractional Crystallization with Special Reference to Element Abundance Relationships

A primary magma not only represents the starting point of a fractional crystallization process,but also is the product of an equilibrium or fractional partial melting process in a mantle. Element abundance relation ships in the primary magma obey both the law of power function for fractional crystallization and the law of fractional linear function for Nullibrium partial melting. Based on this double nature of the primary magma, the authors advanced a principle to restore the primary magma composition from that of an igneous rock series with petrogenesis of fractional crystalization and put forward an approach of estimating the element abundance of the primary magma, exemplified by the rare-earth elements in the Andes volcanic rock series.

分离结晶岩浆岩元素丰度关系定律的事实基础

根据中国西南峨眉山玄武岩一粗面岩系和同源的白马基性超基性岩体的地球化学研究发现:(1)对于分离结晶成因的岩浆岩,元素丰度互呈幂函数关系。报导了这一定律的事实依据,引证了安底斯山脉玄武岩—流纹岩系元素含量数据的系统证实实例。(2)指出:对同源同结晶阶段岩浆岩,元素含量关系有7种基本型式并遵守同一关系式。同源同结晶阶段岩浆岩元素丰度关系式是讨论同源不同结晶阶段岩浆岩元素丰度关系的基础。

多期岩浆分离结晶作用中微量元素丰度关系

本文提出了多期岩浆分离结晶中元素丰度关系的数学表达式;阐述了微量元素正向演化和反向演化的机理;指出了在不同岩浆分离阶段一些微量元素丰度关系常数(R)有明显变化,可以此作为阶段划分的依据。由峨嵋山玄武岩系及基性-超基性层状岩体研究所得出的元素丰度关系式,适用于其他成分岩浆分离结晶成因的岩浆岩系。本文着重列举数据较齐全的智利安底斯山脉玄武岩、玄武安山岩、安山岩、英安岩和流纹岩岩系的资料作为系统验证。

丰度关系法估算分离结晶岩浆岩系原始岩浆成分

幔源原始岩浆是分离结晶过程的起点,又是地幔的平衡或分离部分熔融的产物。在这种原始岩浆岩中元素丰度关系既遵守分离结晶规律（幂函数定律）,又遵守地幔部分熔融规律（分式线性函数或幂函数定律）。根据原始岩浆的元素丰度关系的这种双重特性,以安底斯山脉火山岩系的稀土元素为例,阐明了由分离结晶的岩浆岩岩系成分恢复原始岩浆成分的原理,并厘定出原始岩浆元素丰度的估算方法。

用丰度关系法估计岩浆分离结晶过程的物理化学参数

该文简要介绍了岩浆分离结晶过程中微量元素丰度关系式。讨论了用丰度关系法估计岩浆分离结晶过程中的主要物理化学参数,如元素总分配系数、元素在原始岩浆中的初始含量、分离结晶度等的方法和实际应用。