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银母寺铅锌矿床位于凤(县)太(白)矿田古岔河—殷家坝近东西向复式向斜北翼,次级紧闭线状背斜中。大地构造位置为秦岭褶皱系礼县—柞水冒地槽褶皱带。矿床有用组分以铅锌为主,铜次之。该矿床既具有同生沉积特征,又有后生改造迹象。在凤太矿田几个大中型矿床中还是较典型的,因此了解该矿床的地质特征,探讨矿床成因,具有一定的理论意义和实际意义。
Yinmusi lead-zinc deposit is located in the too (white) ore field of Feng (county) Taibai-Yinjiaba near east-west synclinal syncline north wing, secondary tight linear anticline. The tectonic position of the Qinling Mountains is fold folds of Li County - Zhashui run-trough fold belt. Lead and zinc useful components of the ore-based, followed by copper. The deposit has both syngenetic depositional characteristics, but also signs of retrogressive transformation. It is still typical in several large and medium-sized deposits in Fengtai ore field. Therefore, it is of theoretical and practical significance to understand the geological characteristics of the deposit and explore the genesis of the deposit.