The metallogenesis of Qingchengzi Pb-Zn deposits is controlled by strata and rock formation. The ore deposits are of complex polystage, with three metallogenic epochs during the periods of Paleoproterozoic syn-sedimentation emplacement, Luliangian metamorphic-deformation re-emplacement and Mesozoic tectonomagmatic re-emplacement, respectively. The deposits are genetically stratabound ones with metamorphism-deformation and hydrothermal superimposition on the basis of submarine (spout) hydrothermal deposition, belonging to submarine exhalation sedimentary metamorphic-magmatic hydrothermal reformation type.oft-com:office:office" />