LGRB-BW GK50: Ores and mineral veins
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Tectonic disturbances with gait minerals and alternating grades of ores. Typical mineral veins are fluoride and heavy spit as well as quartz veins. If aisles are considered economically interesting due to their high metal content, it is referred to as veins.
发育有脉石矿物(gangue minerals,原输入疑似笔误为gait minerals)且矿石品位呈交替变化的构造扰动带(tectonic disturbances)。典型矿脉包括氟化物矿脉、重晶石(heavy spar,原输入误写为heavy spit)矿脉以及石英矿脉(quartz veins)。若某一矿化通道因金属品位较高而具备经济开发价值,则将其定义为矿脉。



