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晚元古代青白口纪（晋宁期）华南地区发育着神农架－龙门山－康滇裂谷和东南裂谷系，成为我国重要金矿床形成的时间和空间。２０世纪８０年代以来，已找到一批大、中、小型金矿床，康滇地区也取得较大进展，这些金矿床主要属于层控矿床文章介绍了一些重要的或典型的金矿床的主要地质特征和成矿条件，可供借鉴。最后提出了康滇地区找矿方向和找矿方法。
Late Proterozoic Qingbaikouji (Jinning period) Shennongjia - Longmenshan - Kangdian rift and southeastern rift system developed in southern China, becoming the time and space for the formation of important gold deposits in China. Since the 1980s, a number of large, medium and small gold deposits have been found, and great progress has been made in the areas of Kang and Dian. The gold deposits mainly belong to stratabound deposits. The article introduces the main geological features of some important or typical gold deposits And metallogenic conditions, for reference. In the end, the prospecting direction and ore prospecting method in the Kang-Dian area are proposed.