ore forming fluids 成矿流体
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
Gold ore-forming fluids are characterized by deep-sourced, multi-sourced, and multi-stage.
成矿流体具有深源性、多源性和多期性特征。
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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