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20 0 3年我们课题组在岩浆熔离型金川矿床的深部发现了辉锑矿。辉锑矿是典型的低温热液矿物 ,虽然说岩浆矿床期后或后期也可能有一些热液型矿物出现 ,但在金川岩浆型镍铜硫化物矿床中 ,像辉锑矿这种典型的低温热液矿物还不多见 ,本次尚属首次报道。它的发现 ,突破了原有的金川
In 2030, our research team discovered stibnite in the deep part of magmatic eroded Jinchuan deposit. The stibnite is a typical low-temperature hydrothermal mineral. Although some hydrothermal minerals may appear after or after the magmatic deposit, in the Jinchuan magmatic nickel-copper sulphide deposit, the typical low temperature such as stibnite Hydrothermal minerals are rare, this is the first time reported. Its discovery, broke through the original Jinchuan