First discovery of sedimentary sandstone-hosted rhenium deposit in the Fetianshan Formation (K1f) in the Puge area, Xichang
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图 1 米市盆地地质、铜-铼矿床(点)分布图(a)和矿石(b、c)及镜下照片(d)
1—第四系;2—小坝组;3—飞天山组;4—侏罗系;5—三叠系;6—古生界;7—震旦系;8—南华系;9—断层;10—铜-铼矿床(点)及编号(1—红莫依达矿床;2—白庙子矿点;3—薄日泥堡矿点;4—二虎村矿点;5—轿顶山矿床;6—拉基乡矿点);Bit—沥青;Ce-辉铜矿;Bra—斑铜矿;Mal—孔雀石
Figure 1. Geological map showing distribution of copper-rhenium deposit (spot) (a), ore(b、c)and microscopic photo(d) in Mishi Basin
1-Quaternary; 2-Xiaoba Formation; 3-Feitianshan Formations; 4-Jurassic; 5-Triassic; 6-Paleozoic; 7-Sinian strata; 8-Nanhua system; 9-Fault; 10- copper-rhenium deposit(spots) (1-Hongmoyida spot; 2-Baimiaozi spot; 3-Borinibao spot; 4-Tuomugou Erhu spot; 5-Jiaoding Mountain deposit; 6-Laji spot); Bit-Bitumen; Ce-Chalcocite; Mal-Malachite; Bra-Bornite
表 1 飞天山组含有机质(沥青)条带砂岩矿石铼等元素分析结果
Table 1 Analysis results of rhenium and other elements in organic (bituminous) striped ore of Feitianshan Formation