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矿床地质  2004 

重新认识中国斑岩铜矿的成矿地质条件

Keywords: 地质学,斑岩铜矿,大陆边缘,构造演化,成矿条件,中国

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Abstract:

根据中国大陆洋陆作用的关系和造山带的演化,重新划分了中国斑岩铜矿成矿域和成矿带,将其分为古亚洲、北部特提斯、南部特提斯(喜马拉雅)和环太平洋4个成矿域。古亚洲成矿域又分为华北陆块北缘早_中古生代成矿带、哈萨克斯坦地块东北缘晚古生代成矿带、哈萨克斯坦地块南缘中晚古生代成矿带、西伯利亚板块西南缘晚古生代成矿带。特提斯北部成矿域分为中咱地块西缘晚三叠世义敦成矿带、羌塘地块(昌都_思茅地块)北缘古近纪玉龙成矿带、塔里木地块南缘晚古生代_新生代成矿带、扬子地块西缘古近纪成矿带。南部特提斯(喜马拉雅)成矿域分为班公错成矿带和冈底斯成矿带。环太平洋成矿域分晚中生代活动陆缘成矿带和台湾古近纪_新近纪岛弧成矿带。综合分析中国大陆地质演化史与斑岩铜矿成矿地质背景,对中国斑岩铜矿勘查工作具有重要参考价值。

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