在此基础上，建立了区域中生代构造-流体-成岩成矿地球化学-体化系统模型。
The Mesozoic magmatism and polymetallic mineralization was caused by interaction between deep-derived fluids and Mesozoic multistage tectonic activities.
在此基础上，肯定了成矿流体地球化学在元素共生分异机制研究中的地位和作用。
On the above base, the status and function of fluid geochemistry in studying mechanisms of elemental paragenesis and separation are affirmed.
本区为铜的地球化学高背景场区，具有较好的铜矿成矿条件。
This area is the geochemical one with high copper background value and has the favourable condition for copper mineralization.
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