摘要
<正>作为世界上最重要的铜矿床类型,斑岩铜矿提供了全球约70%的铜资源量(Sillitoe,2010),通常产于与大洋板片俯冲消减作用有关的岛弧和陆缘弧环境(Kerrich et al.,2000;Richards,2003,2012;Cooke et al.,2005;Sillitoe,2010)。然而,最近十多年的研究表明,斑岩铜矿床也可产于陆陆碰撞造山环境中,如产于青藏高原东缘的玉龙斑岩铜钼矿带(Hou et al.,2003;Liang
引文
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