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银洞坡金矿床位于秦岭东西复杂构造带的东段南支，与剪切带的形成、演化密切相关。银洞坡金矿床矿体赋存在特定的构造环境中，以物质流运移的方式，迁移到一定的导矿、容矿构造空间富集成矿，形成的矿体受固定的层位控制。
The Yindongpo gold deposit is located in the southern branch of the eastern segment of the Qinling-West complex belt and is closely related to the formation and evolution of the shear zone. The ore body of the Yindongpo gold deposit exists in a specific tectonic environment and migrates to a certain guide ore by means of material flow. The ore-hosting structure is enriched for mineralization, and the formed ore body is controlled by a fixed horizon.