Ore-forming fluids evolution 成矿流体演化
origin of ore-forming fluids 成矿流体来源
source of ore-forming fluids 成矿流体来源
deep seated ore forming fluids 深源成矿流体
migration of ore forming fluids 成矿流体运移
geochemistry of ore-forming fluids 成矿流体地球化学
The ore forming fluids had very low salinity and could not form oilfield brine.
成矿流体盐度很低，不是高盐度的油田卤水。
This suggests that the different REE fluorites were products of the same source, and REE ore-forming fluids were related to carbonatite and syenite magmas.
这些表明不同稀土特征的萤石来自相同的源区，稀土成矿流体与碳酸岩和正长岩岩浆存在密切联系。
According to calculating other thermodynamic parameters, the ore-forming fluids in ores are characteristic of low-middle salinity, low density and weak deoxidize-deoxidize.
通过对其他热力学参数计算，确定出驼路沟钻矿床成矿流体具有中低盐度、低密度、弱还原-还原性的特点。
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