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作 者:YIN Chao LIU Jiajun ZHAI Degao GUO Yuncheng
机构地区:[1]State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences [2]School of Earth Sciences and Resources, China University of Geosciences
出 处:《Acta Geologica Sinica(English Edition)》2019年第1期241-243,共3页地质学报(英文版)
基 金:supported by the National Natural Science Foundation of China(grants No.41573036 and 41730426);Fundamental Research Funds for the Central Universities,China University of Geosciences(grant No.2652017263)
摘 要:The Dahu quartz vein-style Au-Mo deposit is an important deposit in the Xiaoqingling region,which contains a total reserves of 38 tons of Au at an average grade of 6.8 g/t and 100,000 tons of Mo at an average grade of 0.24%.It is hosted in the highly metamorphic gneiss of the Archaeozoic Taihua group,and the ore-bearing quartz veins are controlled by several small to medium size E–W-striking faults,i.e.,F1,F8,F7,F35,F5,and F6 from north to south(Jian et al.,2015).
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