摘要
音频大地电磁测深法是近几十年来发展起来的一种人工交变电磁场源测深技术,对深部矿的探测具有一定优势,利用该方法结合钻孔资料探测了矿区的地层及矿化带的展布,对矿区的下步工作具有一定指导意义。
The audio magnetotelluric sounding method is a kind of artificial alternating electromagnetic field source sounding technology developed in recent decades. It has certain advantages for the detection of deep mines. The method is used to detect the strata and ore of the mining area by combining the borehole data. The distribution of the belt has certain guiding significance for the next step of the mining area.
引文
[1]汤井田,何继善.可控源音频大地电磁法及其应用[M].长沙:中南大学出版社,2005.
[2]陈玉玲,韩凯,陈贻祥,等.2015.可控源音频大地电磁法在岩溶塌陷勘察中的应用[J].地球物理学进展,30(6):2616-2622.