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陕西凤县铅硐山铅锌矿床处于秦岭褶皱系礼县—柞水华力西冒地槽褶皱带。矿床产于古岔河—殷家坝向斜南翼次级构造——铅硐山—水柏沟紧闭倒转背斜西部倾伏端。矿体受其南侧分支构造铅硐山背斜控制。正在评价的Ⅰ、Ⅱ号主矿体产于同一含矿层位,分别位于背斜的北、南两翼(图1),矿体的厚度、产态、品位等均比较稳定,远景可观。该矿床是秦岭中泥
The lead-zinc-lead deposit in Fengxian County, Shaanxi Province, is located in the fold-trough fold belt of the Li County-Zhashui Hualixi Fold System in the Qinling Mountains. Deposits produced in the ancient Chahe - Yinjiaba anticline south wing secondary structure - Lead Hill - Shui Po ditch closure anticline anticline oblique ends. The ore body is controlled by the lead hill anticline on the south branch. The main ore bodies I and II under evaluation are located in the same ore-bearing bed and are respectively located in the north and south wings of the anticline (Figure 1). The thickness, production status and grade of the ore body are relatively stable with long-term prospects. The deposit is mud in the Qinling Mountains