Abstract：The orebodies in the Jinniuchang Pb-Zn deposit occur in the NWW-trending plumose fractures. Study shows that the Pingqing anticline, which is the results of regional NW-SE structural stress, serves as the main ore-controlling structure. The NE-trending Guancangqing reverse fault is the passage-way for ore fluid. The secondary NWW-trending tenso-shearing fault is the main host structure. The orebodies are obviously controlled by structures in the orefield, therefore the deep and surrounding areas are prospective for ore-searching.
洪建磊, 程云茂, 范良军, 苏昌学. 云南省会泽县金牛厂铅锌矿构造控矿特征及找矿方向[J]. 地质与资源, 2017, 26(3): 260-264.
HONG Jian-lei, CHENG Yun-mao, FAN Liang-jun, SU Chang-xue. STRUCTURAL CONTROLLING CHARACTERISTICS AND PROSPECTING GUIDE OF THE JINNIUCHANG LEAD-ZINC DEPOSIT IN HUIZE COUNTY, YUNNAN PROVINCE. GEOLOGY AND RESOURCES, 2017, 26(3): 260-264.
2017, Vol. 26 
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