地球化学场是由地质地球化学作用形成的各种地球化学指标的特征变化空间。
研究区域地球化学场可用区域分散流普查资料来进行。
Regional stream sediment data can be used in studies of regional geochemical fields.
金的区域地球化学场分布受断裂构造、地层及岩浆岩控制。
The distribution of the regional geochemical field of gold is controlled by fault structure, stratum and intrusive rocks.
区域地球化学场趋势显示了该区为钨、金、铜矿化集中区的特征。
The trend of regional geochemical field shows that the area is characterized by tungsten, gold, copper mineralization.
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