Abstract:The Dapingzhang Cu-polymetallic deposit is a typical volcanic exhalative sedimentary deposit in western Yunnan. This paper has summarized the geophysical characteristics of the ore district and established the geophysical anomaly model for the Dapingzhang deposit in combination with the geological features, in the hope that the model can guide the prospecting work in the depth and on the periphery of the ore district. In this paper, the main geological features include IP intermediate gradient anomaly, IP sounding anomaly, high-frequency magnetotelluric method (EH-4) anomaly and Transient Electromagnetic Method (TEM) anomaly in the ore district.
袁小龙, 李文尧, 李峰, 罗安华, 郭亮. 滇西大平掌铜多金属矿地球物理特征及异常模型[J]. 物探与化探, 2013, 37(5): 817-821.
YUAN Xiao-long, LI Wen-yao, LI Feng, LUO An-hua, GUO Liang. GEOPHYSICAL CHARACTERISTICS AND ANOMALY MODEL OF THE DAPINGZHANG Cu-POLYMETALLIC DEPOSIT IN WESTERN YUNNAN. Geophysical and Geochemical Exploration, 2013, 37(5): 817-821.