Siliceous dolostone, lime dolostone, moyite and volcanic detrital rocks are the mainhostrocks of the mineral water.
本矿泉水赋存岩石为硅质白云岩、灰质白云岩、钾长花岗岩和火山碎屑岩。
There is variation of geochemical composition in the different stage moyite, which will help us to understand the evolution of the crustal composition and movement in the time.
根据不同期次钾长花岗岩在地球化学组分方面存在的差异变化，有助于了解地壳成分及地壳构造运动在时间上的演化。
There is variation of geochemical composition in the different stage moyite, which will help us to understand the evolution of the crustal composition and movement in the time.
根据不同期次钾长花岗岩在地球化学组分方面存在的差异变化，有助于了解地壳成分及地壳构造运动在时间上的演化。
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