内蒙古狼山造山带构造演化与成矿响应

彭润民 翟裕生 韩雪峰 王志刚 王建平 沈存利 陈喜峰. 内蒙古狼山造山带构造演化与成矿响应[J]. 岩石学报, 2007, 23(3): 679-688.
引用本文: 彭润民 翟裕生 韩雪峰 王志刚 王建平 沈存利 陈喜峰. 内蒙古狼山造山带构造演化与成矿响应[J]. 岩石学报, 2007, 23(3): 679-688.
Mineralization response to the structural evolution in the Langshan orogenic belt, Inner Mongolia[J]. Acta Petrologica Sinica, 2007, 23(3): 679-688.
Citation: Mineralization response to the structural evolution in the Langshan orogenic belt, Inner Mongolia[J]. Acta Petrologica Sinica, 2007, 23(3): 679-688.

内蒙古狼山造山带构造演化与成矿响应

  • 基金项目:

    国家自然科学基金项目(批准号:40572064)、国家自然科学重点基金项目(批准号:40234051)、国家重点基础研究发展计划项目(编号2006CB403503)和内蒙古自治区地质勘查招标项目(编号:2004-01-KY2)联合资助.

Mineralization response to the structural evolution in the Langshan orogenic belt, Inner Mongolia

  • 狼山造山带位于华北地台北缘西段,它经历了新太古代和古元古代结晶基底形成与变形、中元古代被动陆缘裂陷槽裂解→沉积→闭合、新元古代晚期开始的活动陆缘、海西期-中生代以来的挤压造山并伴有大量中酸性岩浆侵入的漫长构造演化与发展过程.该造山带有丰富的锌、铅、铜、铁、金等矿产资源,矿床(化)类型、矿床规模与时空分布规律都与其成矿地质背景、构造演化有密切的耦合关系,在不同构造演化阶段有不同的矿床形成:在新太古代主要形成了海底火山环境热水沉积条带状铁矿、在中元古代主要形成了与被动陆缘裂解过程相关的海底喷流-沉积铅锌铜铁硫化物矿床、而在海西期-中生代以来挤压造山过程中的岩浆热液活动,既形成了中小型的斑岩型铜金矿床、又对中元古代等先成的喷流-沉积矿床产生了明显的改造和叠加成矿作用.东升庙、炭窑口和霍各乞矿床的部分铜矿是造山过程中叠加成矿的结果.
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修回日期:  2006-09-24
刊出日期:  2007-03-31

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