In the model, isotopicexchange probability is variable and other parameters come from reference or experiment.
模型中的气-固相同位素交换几率为可变参数,其余参数使用了文献值或实验值。
2
Oxygen diffusion in minerals and accompanied isotopicexchange inclosed systems are discussed with special application to geospeedometry.
概述了同位素封闭体系内的矿物氧扩散和同位素交换机制及其在地质速率计上的应用。
3
The s isotopic components of metal minerals indicates a mid-low-temperature environmental precipitation under the condition of isotopicexchange equilibrium.