吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (6): 1879-1885.doi: 10.13278/j.cnki.jjuese.201506306
• 地球探测与信息技术 • 上一篇
欧阳菲1,2, 罗先熔2, 付立春3
Ouyang Fei1,2, Luo Xianrong2, Fu Lichun3
摘要:
笔者以湖南大根垄钨多金属矿为试验研究区,以20 m点距在已知矿体上方取土壤样,并按照24 h提取时间、1 000 mL HNO3提取液、50 cm电极间距等工作条件进行了地电提取试验。结果表明,地电提取前后土壤中的元素含量变化不大,被提取到的金属元素应属土壤金属总量的一部分。次生晕与地电提取的异常形态对比发现:Co、Ni较清晰,W次之,Cr无异常;元素的异常特征主要取决于土壤中该元素的活性形式所占比例。综合分析认为地电提取异常与矿体的相对位置有关:矿体的下坡位置以及控矿断裂附近容易形成异常,距离原生矿体太近则会对异常有明显干扰。在本矿区,矿体风化程度越高对Co、Ni的地电提取异常越有利;其异常宽度一般比次生晕窄。
中图分类号:
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