Diaobingshan wollastonite deposit is a super-large ore deposit. Regionally, it occurs in middle of the east ore belt. There are three ore blocks of which Dongquangou block is closely controlled. Wollastonite ore bodies are mainly in silicified marble of Paleozoic Fulabuzi Formation trending NNE and dipping to SE. They are controlled by horizon, lithology and magmatic rock. The ore belt is 2 000 m long with outcrop 14~65 m wide and by-products of Au, Mo, Pb, Zn and Ag. Because physical property of the ore body is quite varied with that of the wall-rock three IP intermediate gradient sections are selectively surveyed at the area with sedimentary cover and three resistivity anomaly trending NNE are located.