CAJ | 학술논문

昆山矿区位于赣北九岭成矿带中段，大湖塘矿田南部，具有优越的成矿地质条件。自1967年起由昆山钨矿开采，2008年以后，矿山处于停产状态。前人地质找矿历经20余年，但受计划经济等因素制约，地质找矿始终未有大的突破。这次找矿，通过矿权的整合、社会资本的投入、找矿思路的转变，取得了重大进展。目前矿区勘查仍在进行，通过这次工作，发现了一个中－大型石英脉带型钼钨铜矿床，钼、钨有望达到大型规模，铜达到小型规模。
곤산광구위우공북구령성광대중단，대호당광전남부，구유우월적성광지질조건。자1967년기유곤산오광개채，2008년이후，광산처우정산상태。전인지질조광력경20여년，단수계화경제등인소제약，지질조광시종미유대적돌파。저차조광，통과광권적정합、사회자본적투입、조광사로적전변，취득료중대진전。목전광구감사잉재진행，통과저차공작，발현료일개중－대형석영맥대형목오동광상，목、오유망체도대형규모，동체도소형규모。
Kunshan mining area is located in the middle of Jiuling metallogenic belt of northern region of Jiangxi and in the south of Dahutang tungsten orefield.Its metallogenic geological conditions are advantageous.The orefiled was exploited since 1967 to 2008.Because of the planned economy, the geological prospecting of this orefield did not a-chieve break-through after more than twenty years ’ work.Nevertheless, we have made significant progress re-cently, through the integration of mining rights, the market investment and the transformation of prospecting idea. We have discovered a medium to large-scale Mo-W-Cu ore deposit of quartz vein type now.Currently, Mo-W ore deposit is expected to reach a large scale and copper ore deposit is expected to reach a small scale.