Abstract:Maoling gold deposit,located in the southwest of Liaodong Peninsula, discovered in 1985, is a giant veinlet-disseminated ore with low grade. The ore bodies are auriferous quartz veinlets and-arsenopyritized-pyritized sericite phyllite or schist. Au grade ranges from 3 to 5g/t. The country rock is the second member of Gaixian formation. Magmatic activities were common in the area.
刘斌, 余昌涛. 辽南猫岭细脉浸染型金矿床的成矿模式[J]. 地质与资源, 1994, 3(2): 103-106.
Liu Bin, Yu Changtao. THE METALLOGENIC MODEL FOR MAOLINGVEINLET-DISSEMINATED GOLD DEPOSITIN THE SOUTH LIAONING. GEOLOGY AND RESOURCES, 1994, 3(2): 103-106.