The effect of applying audio-frequency magnetotelluric method to the deep geological exploration: A case study of Wushan periphery in the Jiurui ore concentration area
YAO Da-Wei1,2, ZHU Wei1, WANG Da-Yong1, WANG Gang1, ZHANG Zhen-Yu1
1. National Center of Geological Exploration Technology, Institute of Geophysical and Geochemical Exploration, CAGS, Langfang 065000, China;
2. School of Geophysics and Information Technology, China University of Geosciences, Beijing 100083, China
According to the geological background, metallogenic conditions and petrophysical characteristics in the surveyed area, three-dimensional geological mapping was studied by Audio-frequency Magnetotellurics Method (AMT). Based on AMT raw data processing and inversion interpretation, the authors inferred the underground resistivity differences of lithology and fracture structure within 2 km from the contact zone. Combined with the geological data and drilling results, the authors hold that the audio magnetotelluric method is good for detecting the underground geological body, clearly recognizing the marker bed of geoelectric layer and its hierarchical structure.
姚大为, 朱威, 王大勇, 王刚, 张振宇. 音频大地电磁法在武山外围深部勘查中的应用[J]. 物探与化探, 2015, 39(1): 100-103.
YAO Da-Wei, ZHU Wei, WANG Da-Yong, WANG Gang, ZHANG Zhen-Yu. The effect of applying audio-frequency magnetotelluric method to the deep geological exploration: A case study of Wushan periphery in the Jiurui ore concentration area. Geophysical and Geochemical Exploration, 2015, 39(1): 100-103.