The isotopic composition of oxygen shows that the origin of the ore forming solution was turn from magmatic water in early stage to circulated meteoric water in later stage.
通过氧同位素研究证明了成矿溶液的来源由早期岩浆水转变为晚期大气降水；
The isotopic composition of oxygen shows that the origin of the ore forming solution was turn from magmatic water in early stage to circulated meteoric water in later stage.
通过氧同位素研究证明了成矿溶液的来源由早期岩浆水转变为晚期大气降水；
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