初论环准噶尔斑岩铜矿带的地质构造背景与形成机制

董连慧, 徐兴旺, 屈迅, 李光明. 初论环准噶尔斑岩铜矿带的地质构造背景与形成机制[J]. 岩石学报, 2009, 25(4): 713-737.
引用本文: 董连慧, 徐兴旺, 屈迅, 李光明. 初论环准噶尔斑岩铜矿带的地质构造背景与形成机制[J]. 岩石学报, 2009, 25(4): 713-737.
DONG LianHui, XU XingWang, QU Xun, LI GuangMing. Tectonic setting and formation mechanism of the circum-Junggar porphyritic copper deposit belts[J]. Acta Petrologica Sinica, 2009, 25(4): 713-737.
Citation: DONG LianHui, XU XingWang, QU Xun, LI GuangMing. Tectonic setting and formation mechanism of the circum-Junggar porphyritic copper deposit belts[J]. Acta Petrologica Sinica, 2009, 25(4): 713-737.

初论环准噶尔斑岩铜矿带的地质构造背景与形成机制

  • 基金项目:

    中国科学院知识创新工程主要方向项目(KZCXZ-YW-107)、“十一五”国家科技支撑计划重点项目(2006BAB07B01-03)与中国科学院矿产资源重点实验室基金

Tectonic setting and formation mechanism of the circum-Junggar porphyritic copper deposit belts

  • 准噶尔地区构造-岩浆-成矿带具环准噶尔地块分布的特征,这一格局是准噶尔地区古生代大地构造演化的结果。哈萨克斯坦-准噶尔板块在北侧古亚洲洋与南侧南天山洋的俯冲下不断侧向增生,并形成与岩浆作用伴生的火山岩型铜铁多金属矿带、斑岩铜钼金矿带与浅成低温金矿带。哈萨克斯坦-准噶尔板块与西伯利亚板块和塔里木板块碰撞发生了强烈挤压-剪切变形,并导致准噶尔地块发生逆时针旋转,从而造成构造-岩浆-成矿带发生位移、呈环状分布于准噶尔地块周边。环准噶尔斑岩铜矿形成于俯冲成因的大陆岛弧、大洋岛弧与弧后盆地及后碰撞阶段板内4种构造背景,晚古生代是成矿的高峰时期。
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出版历程
收稿日期:  2008-10-21
修回日期:  2009-02-19
刊出日期:  2009-04-30

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