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The Baoshan Cu-Pb-Zn polymetallic deposit is lied in the central Nanling mineralization zone,and belongs to the junction area of the Chenzhou-Linwu fault zone and the Leiyang-Linwu fault zone.It is a significant part of Nanling polymetallic deposit belt.The outcropping stratas consist of upper Devonian Shetianqiao,Xikuangshan Formation,Lower Carboniferous Menggong’ao,Shidengzi,Ceshui,and Zimenqiao Formation.Igneous rocks in the Baoshan ore area mainly comprise granodiorite porphyry.Furthermore,the radio isotopic age ranges from 123 Ma to 183 Ma,belonging to the early to middle Yanshanian.
The Baoshan Cu-Pb-Zn polymetallic deposit is lied in the central Nanling mineralization zone, and belongs to the junction area of the Chenzhou-Linwu fault zone and the Leiyang-Linwu fault zone. It is a significant part of the Nanling polymetallic deposit belt. The outcropping stratas consist of upper Devonian Shetianqiao, Xikuangshan Formation, Lower Carboniferous Menggong’ao, Shidengzi, Ceshui, and Zimenqiao Formation. Igneous rocks in the Baoshan ore area predominantly granodiorite porphyry. Future plus, the radio isotopic age ranges from 123 Ma to 183 Ma, belonging to the early to middle Yanshanian.