The Qinling-type lead and zinc ore deposit is located in the Qinling fold belt, occurring in the Devonian marine fine clastic and carbonate rocks. It is a sedimentary-reworked ore deposit which is basically a sedimentary deposit further hydrothermally ref
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李健中 何典仁.1992.秦岭型铅—锌矿床[J].地质学报,66(3). Li Jianzhong.1992. THE QINLING-TYPE LEAD AND ZINC ORE DEPOSIT[J]. Acta Geologica Sinica,66(3).
