| 祁漫塔格地区构造-岩浆作用与成矿 |
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| 引用本文： | 高晓峰,校培喜,谢从瑞,过磊,董增产,奚仁刚,康磊.祁漫塔格地区构造-岩浆作用与成矿[J].西北地质,2010,43(4):119-123. |
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| 作者姓名： | 高晓峰 校培喜 谢从瑞 过磊 董增产 奚仁刚 康磊 |
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| 作者单位： | 中国地质调查局西安地质调查中心,陕西西安710054 |
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| 基金项目： | 中国地质调查局国土资源大调查项目 |
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| 摘 要： | 对祁漫塔格地区构造-岩浆作用的研究表明,岩浆活动峰期为加里东期—印支期,并有从北向南逐渐变新的趋势。区域成矿峰期与岩浆活动峰期是一致的,主要成矿母岩为岩浆弧相俯冲-碰撞杂岩。另外,祁漫塔格地区主要发育北东向和北西向两组断裂带,北东向断裂是影响区域成矿的主控因素。
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| 关 键 词： | 构造特征 岩浆岩 祁漫塔格 东昆仑 |
Discussion on Tectonic-Magmatic Process and Mineralization in the Qimantage Region |
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| GAO Xiao-feng,XIAO Pei-xi,XIE Cong-rui,GUO Lei,DONG Zeng-chan,XI Ren-gang,KANG Lei.Discussion on Tectonic-Magmatic Process and Mineralization in the Qimantage Region[J].Northwestern Geology,2010,43(4):119-123. |
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| Authors: | GAO Xiao-feng XIAO Pei-xi XIE Cong-rui GUO Lei DONG Zeng-chan XI Ren-gang KANG Lei |
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| Institution: | (Xi＇an Center of Geological Survey,CGS,Xi＇an 710054,China) |
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| Abstract: | The Qimantage Mountains region is a part of the East Kunlun multi-stage composite orogenic belt and important source of mineral resources;therefore how to analyze and understand the geological background of the deposit is necessary.According to the regional tectonic evolution and deep geodynamics,sedimentary rock formation and the characteristics of temporal and spatial distribution of magmatic rocks and tectonic magmatism process and so on,in this article,the Qimantage regional geological background has been discussed;a number of views for further geological research and prospecting work have been brought forward;and some basic information of geology and specific ideas have been provided. |
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| Keywords: | structure characters igneous rocks Qimantage East Kunlun |
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