• 责任者：Shen Xiaoming (Key Laboratory of Crustal Dynamics ; Institute of Crustal Dynamics ; China Earthquake Administration ; Beijing 100085 ; China) ; Luo Xianrong
• 刊名：Geoscience
• 出版年：2013
• 卷期：27(4)
• 关键词：锑矿 ; antimony ores ; 射气测量 ; emanation surveys ; 云南 ; Yunnan Province
• 页码：p.799-808
• 图表：7 illus., 1 table, 16 refs.
• 分类号：1600
• issnNo：ISSN1000-8527
• isbnNo：CN11-2035/P

     The Muli antimony ore bodies in Yunnan have close relationship with the faults. The data indicate that all of the known faults (including faults of Xiaopunong, F1, F2 and F3) and ore bodies show clear radon anomaly. It is suggested that the radon measurement may be an effective method to search for buried faults and an auxiliary method to search for buried deposits which have close relationship with the fracture structure including faults, joints and cleavages. The results reveal that there are two large buried faults in the core of the anticline and the northeastern study area, respectively, and there are many secondary faults of the known faults and the predicted faults. In the end, the radon anomaly model of the study area is summarized.