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礼岷前陆盆地经历了早期深海—半深海的复理石沉积阶段和晚期陆相磨拉石沉积阶段。该盆地在成盆及盆山转换过程中在其前渊、隆后盆地以及褶皱冲断带内形成了Au、Ag、Pb、Zn、Cu、Mo等多金属矿床。
The Li Min foreland basin experienced the stages of the early deep-semi-deep sea dolomitic sedimentary stage and the late terrestrial molasse sedimentary stage. The basin formed Au, Ag, Pb, Zn, Cu, Mo and other polymetallic deposits in the foreland basin, the Longmen basin and the fold-thrust belt during the basin-basin and basin-level conversion.