The source of uranium is mainly due to magmatic differentiation.
铀源主要来自岩浆分异。
It has characteristics of polystage-magmatic intrusions, polystage metallogenetic evolution and zonal differentiation of the ore deposit.
具有多阶段岩浆侵入,多阶段成矿演变及矿床带状分异的特征。
It has characteristics of polystage-magmatic intrusions, polystage metallogenetic evolution and zonal differentiation of the ore deposit.
具有多阶段岩浆侵入,多阶段成矿演变及矿床带状分异的特征。
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