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在成矿过程中,铼主要同钼而较少同其他金属聚集在一起。铼的矿物富集体主要是辉钼矿,其次是黄铜矿、斑铜矿、黄铁矿、方铅矿及其他矿物。独立的铼矿物十分罕见。虽然有关文献在讨论不同成因辉钼矿中铼的聚集和分布特点方面存在着不同观点,但仍可提出以下一些普遍规律。低温矿床辉钼矿中铼的高含量要比高温矿床辉钼矿中常见得多。铜-钼矿床中的辉钼矿要比铝矿床本身、钨-钼矿床及伟晶岩石中的辉钼矿更富铼。在同一矿床中,铼常常趋于在上部的钼矿石中优先富集。这对于在下部发育有辉钼矿与白钨矿、钼自钨
During mineralization, rhenium is mainly associated with molybdenum and less with other metals. Rhenium minerals are mainly molybdenite, followed by chalcopyrite, bornite, pyrite, galena and other minerals. Independent rhenium minerals are very rare. Although there are different opinions on the characteristics of rhenium accumulation and distribution in molybdenites of different genetic origins, some general laws may still be proposed. The high content of rhenium in low-temperature molybdenite ore is much more common than the high-temperature molybdenite ore. The molybdenite in the copper-molybdenum deposit is richer than the molybdenite itself, tungsten-molybdenum deposit and molybdenite in pegmatite. In the same deposit, rhenium tends to preferentially enrich in the upper molybdenum ore. This is for the lower part of the development of molybdenite and scheelite, molybdenum from tungsten