Abstract：The Shengou gold-antimony deposit, located in the western section of Middle Qilian metallogenic belt in Qinghai Province, belongs to Middle Qilian-Taibai formation subarea in terms of stratigraphic division. On the basis of field survey and test analysis, with comprehensive study on stratigraphy, lithology, structural conditions and magmatic rocks, it is considered that the deposit belongs to meso-epithermal mineralization with ore-orming fluids mainly of magmatic vapor-water and underground hydrates. The orebody occurrences are controlled by both structural fracture belts and rock mass. With multiple differentiation and enrichment of ore-forming elements due to multi-stage tectonic activity, the high grade gold-antimony deposit is formed with prospecting potential.
神元, 刘向阳, 莫家琛, 翟亚锋, 张睿, 彭琼斌, 孙雨. 中祁连西段深沟金锑矿床地质特征及找矿方向探讨[J]. 地质与资源, 2018, 27(1): 54-59.
SHEN Yuan, LIU Xiang-yang, MO Jia-chen, ZHAI Ya-feng, ZHANG Rui, PENG Qiong-bin, SUN Yu. GEOLOGY AND PROSPECTING DIRECTION OF SHENGOU GOLD-ANTIMONY DEPOSIT IN THE WESTERN SECTION OF MIDDLE QILIAN MOUNTAINS. GEOLOGY AND RESOURCES, 2018, 27(1): 54-59.
2018, Vol. 27 
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