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四川会东麦地铅锌铜矿是近年来新发现的一中型多金属矿床,是扬子地台西缘较为典型热液层控型矿床(MVT型)。矿床明显受地层、构造双重控制,与麦地坪组、灯影组及发育在其中层间破碎带、构造裂隙有关。通过对麦地铅锌铜矿的矿床地质特征、控矿因素及找矿标志等分析和研究,提出了区内该类矿床找矿方向。
The lead-zinc-copper mine in eastern Huidong, Maize, is a newly discovered medium-sized polymetallic deposit in recent years. It is a typical type of thermohydraulic stratiformization deposit (MVT) in the western margin of the Yangtze platform. The deposit is obviously controlled by the strata and structure, which are related to the MaiDipiping Formation, the Dengying Formation and the interlaminar crustal zone and structural fissure in it. Based on the analysis and research on the geological characteristics, ore-controlling factors and prospecting signs of the Maidi lead-zinc-copper deposit, the prospecting direction of this kind of ore deposits in the area is proposed.