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四川攀枝花云鹿铜铂金矿区是一个新发现的比较罕见的新类型含铂族元素矿床,其特殊性至少表现为:矿化体赋存在炭质岩系中、炭质岩系中富含镁电气石(MgO含量7.68%~8.64%,平均8.15%)、表生过程中低温条件下铂族元素发生了活化转移(含铜钟乳石中含PGE0.14×10-6)。铂族元素的最初富集可能与元古宙的海底喷气活动有关。此类铂族元素的矿化在国内外罕见,有可能是第一次发现,但类似的成矿地质条件在中国西南地区普遍存在,应该在今后的地质研究与找矿过程中加以注意。
Sichuan Panzhihua Yunlu copper-platinum deposit is a newly discovered relatively rare new type of platinum-bearing group ore deposit. Its peculiarities are at least as follows: the mineralized deposit exists in the carbonaceous rock series, and the carbonaceous rock series is rich in magnesium electric (MgO content 7.68% ~ 8.64%, average 8.15%). During the epidural process, the platinum group elements were activated and transferred under the low temperature condition (PGE 0.14 × 10-6 in copper-bearing stalactites). The initial enrichment of platinum group elements may be related to the Proterozoic submarine jet activity. The mineralization of such platinum group elements is rare at home and abroad, and may be the first discovery, but similar metallogenic geological conditions prevail in southwestern China and should be paid attention to in the future geological research and prospecting process.