同位素交换 isotopic exchange
- 碱性长石流体的氧同位素交换机制主要是溶解再沉淀。
The mechanism of oxygen isotope exchange between alkali feldspar and fluid is mainly dissolution reprecipitation. - 金属矿物硫同位素组成在同位素交换平衡条件下属中低温环境沉淀。
The s isotopic components of metal minerals indicates a mid-low-temperature environmental precipitation under the condition of isotopic exchange equilibrium. - 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。
In the model, isotopic exchange probability is variable and other parameters come from reference or experiment.
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