摘要
微量元素协变方程的系数与该元素的分配系数之关系因其描述的成岩过程不同而异．据此，可以在已知分配系数的条件下识别协变方程，从而推测成岩过程；也可在已知成岩过程的条件下，推测微量元素的分配特征．
The relationship between the coefficient of the microelement covariant-equation and the distribution coefficient varies with the different magmatic processes.According to this,identifying the covariant-equation from the known distribution coefficient can be made.Therefore,the magmatic process can be inferred, Under the condition of the known magmatic process,the distribution characteristics of mictoelements can be also inferred.
出处
《桂林工学院学报》
1995年第4期419-424,共6页
Journal of Guilin University of Technology
