2013年第4期目录
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封面故事：西藏尕尔穷铜金矿床的铁氧化物-铜-金建造型矿体及ZK2101钻孔202.4m处的自然金。尕尔穷铜金矿位于班公湖-怒江结合带南缘，为缝合带构造演化过程中碰撞期成矿事件的典型代表。高品位富金的铁氧化物-铜-金建造型矿体的发现提高了该矿床的经济价值、为区域找矿工作提供新的方向，同时也丰富和完善了西藏斑岩型矿床的矿体类型组合及矿床成矿系列理论。这项由中国地质科学院矿产资源研究所唐菊兴研究员主持的研究成果，当选2012年度中国地质科学院十大科技进展，排名第八。详见本期385-394页。（图片提供：唐菊兴、张志）
Cover Story：The iron oxide-copper-gold formation type ore body and native gold at the depth of 202.4m of borehole ZK2101 in the Ga’erqiong deposit, Tibet. Located on the southern margin of the Bangong Lake-Nujiang River juncture belt, the deposit is the typical representative of the metallogenic event of the suture belt during the collision period in the process of the tectonic evolution. The discovery of the high-grade gold-rich iron oxide-copper- gold formation type ore body has greatly improved the economic value of this ore deposit, provided new orientations for regional prospecting work, and also enriched and perfected the ore body type assemblage and metallogenic series theory of ore deposit. The research achievement led by Professor TANG Ju-xing, Institute of Mineral Resources, CAGS, ranks the eighth among “Top Ten Scientific and Technological Progresses of CAGS in 2012”. For details, see page 385-394 of this issue. (Photo by TANG Ju-xing and ZHANG Zhi)
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