哈萨克斯坦环巴尔喀什斑岩铜矿地质与成矿背景研究

李光明, 秦克章, 李金祥. 哈萨克斯坦环巴尔喀什斑岩铜矿地质与成矿背景研究[J]. 岩石学报, 2008, 24(12): 2679-2700.
引用本文: 李光明, 秦克章, 李金祥. 哈萨克斯坦环巴尔喀什斑岩铜矿地质与成矿背景研究[J]. 岩石学报, 2008, 24(12): 2679-2700.
LI GuangMing, QIN KeZhang, LI JinXiang. Geological features and tectonic setting of porphyry copper deposits rounding the Balkhash region, Central Kazakhstan, Central Asia[J]. Acta Petrologica Sinica, 2008, 24(12): 2679-2700.
Citation: LI GuangMing, QIN KeZhang, LI JinXiang. Geological features and tectonic setting of porphyry copper deposits rounding the Balkhash region, Central Kazakhstan, Central Asia[J]. Acta Petrologica Sinica, 2008, 24(12): 2679-2700.

哈萨克斯坦环巴尔喀什斑岩铜矿地质与成矿背景研究

  • 基金项目:

    国家科技支撑计划重点项目(2006BAB07B08)和中国科学院知识创新方向项目(KZCX2-YW-107)资助

Geological features and tectonic setting of porphyry copper deposits rounding the Balkhash region, Central Kazakhstan, Central Asia

  • 中哈萨克斯坦位于中亚造山带中部,是中亚型造山带及中亚斑岩铜矿成矿域的重要组成部分,已发现数十个大型和超大型矿床,成群成带分布。主要的斑岩铜矿类型有斑岩铜-金矿、斑岩铜矿、斑岩铜钼矿,大多具同期火山岩。已建立的热液蚀变分带模式具有碱性蚀变和酸性蚀变两个阶段,已有的硫铅同位素数据表明成矿物质来源于深部。该地区的斑岩铜矿形成与多阶段构造演化有关,早古生代的斑岩铜矿与岛弧演化的早阶段有关,而晚古生代的斑岩铜矿与泥盆纪火山—岩浆弧、石炭纪—二叠纪的火山—岩浆弧有关。从中哈萨克斯坦的北西向南东方向,斑岩铜矿的形成时代逐渐变年轻。虽然经过数十年的研究,但该地区的有关斑岩铜矿的精细时空结构仍未建立。因此,含矿斑岩体与蚀变矿化年龄的精确测定、区域成矿地球动力学背景及其演化、斑岩铜矿的精细时空结构、与中国邻区的构造—岩浆—成矿带的连接对比将是以后的研究方向。
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出版历程
收稿日期:  2008-06-20
修回日期:  2008-09-08
刊出日期:  2008-12-31

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