摘要
As Pujue manganese ore field is heavily covered by arid regolith,it’s very hard to determine the geological structure line.In order to investigate the hidden fault characters and manganese ore bed distribution from Jianshan to Houjiazhuang,the magentotelluric depth sounding is done to one section,the geophysical anomaly show that F1 fault plane is noncontinuous plane from low resistivity to high resistivity,it distributes almost vertically as crinkle.The geophysical anomaly also shows the eastern manganese bearing stratum of F1 fault has anticline-syncline structure and the anticlinal axis is inverse.The test shows EH4 geophysical prospecting method has guiding significance for determine the deep hidden geologic structure in this area.