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康定碳酸盐岩石中层控型金矿,远景可观,矿床类型新颖。它的发现,在四川金矿地质工作中无疑是一项新的突破。一,矿床产出的地质环境康定金矿区在大地构造分区上位于扬子准地台康滇地轴北段的西缘,与松潘甘孜褶皱系毗邻。在区域构造上位于康定大断裂的侧旁,界于郭达山断裂及杨康坝断裂之间;滑山向斜的东翼。区内地层不整合超覆于澄江——晋宁期花岗岩之上,依次出露震旦系上统陡山沱
Kangding carbonate rock middle controlled gold mine, a long-term prospect, the deposit type novel. Its discovery is undoubtedly a new breakthrough in the geological work of gold mines in Sichuan. First, the geological environment of the output of the deposit Kangding gold mining area in the tectonic division of the Yangtze River is located in the western margin of Kangdian north axis, adjacent to the Songpan Ganzi fold system. It is located on the side of the Kangdingda fault in the tectonic setting, between the Gudaoshan fault and the Yangkangba fault, and eastward of the syncline. The unconformity of the strata overlies the Chengjiang-Jinning granite, which in turn reveals the Upper Sinian Doushan