| 西藏甲玛-卡军果推-滑覆构造系特征 |
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| 引用本文： | 钟康惠,李磊,周慧文,白景国,李伟,钟婉婷,张勇强,蔺吉庆,郑凡石,黄小雨,陆彪,雷波.西藏甲玛-卡军果推-滑覆构造系特征[J].地球学报,2012,33(4):411-423. |
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| 作者姓名： | 钟康惠 李磊 周慧文 白景国 李伟 钟婉婷 张勇强 蔺吉庆 郑凡石 黄小雨 陆彪 雷波 |
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| 作者单位： | 成都理工大学地球科学学院；国土资源部构造与成矿成藏重点实验室;中国地质科学院矿产资源研究所;海南省地质调查院;四川省冶金地质勘查院;安徽省地质调查院;成都理工大学地球科学学院;成都理工大学地球科学学院;成都理工大学地球科学学院;成都理工大学地球科学学院;成都理工大学地球科学学院;成都理工大学地球科学学院;成都理工大学地球科学学院 |
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| 基金项目： | 国家973项目(编号: 2011CB403103)；地质调查项目(编号: 1212011221073; 1212011086057)；“十一五”国家科技支撑计划项目(编号: 2006BAB01A04-4; 2006BAB01-05～06) |
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| 摘 要： | 通过矿区填图和路线调查,结合室内研究,指出:①甲玛-卡军果推-滑覆构造系由印度-欧亚板块碰撞引发,具有递进变形、自盆地中心向边部推覆、新盖老等特点,强变形于50Ma±。②推覆体下盘为叶巴组构造岩系;推覆体由上侏罗统和下白垩统碳酸盐-碎屑沉积岩系构成,主体为轴面北倾的复式褶皱,自南而北分为前部带、中部带和后部带。滑覆构造系推覆形成的复背斜轴部高位岩块失稳向北滑覆形成,自南而北分为后部带、中部带和前部带。③导致矿区蚀变的主要岩浆活动发生于推覆强变形后的松弛期,上侵受近南北向基底断裂和推覆断裂联合控制,就位受控于前部带推-滑覆褶断系,其后发生多次构造-岩浆-成矿液叠加,造就甲玛铜多金属矿床。
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| 关 键 词： | 西藏甲玛-卡军果推-滑覆构造系 构造特征 形成机制 形成时代 控岩控矿 |
Features of Jiama(Gyama)-Kajunguo Thrust-gliding Nappe Tectonic System in Tibet |
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| ZHONG Kang-hui,LI Lei,ZHOU Hui-wen,BAI Jing-guo,LI Wei,ZHONG Wan-ting,ZHANG Yong-qiang,LIN Ji-qing,ZHENG Fan-shi,HUANG Xiao-yu,LU Biao and LEI Bo.Features of Jiama(Gyama)-Kajunguo Thrust-gliding Nappe Tectonic System in Tibet[J].Acta Geoscientia Sinica,2012,33(4):411-423. |
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| Authors: | ZHONG Kang-hui LI Lei ZHOU Hui-wen BAI Jing-guo LI Wei ZHONG Wan-ting ZHANG Yong-qiang LIN Ji-qing ZHENG Fan-shi HUANG Xiao-yu LU Biao and LEI Bo |
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| Institution: | 1) 1) College Of Earth Sciences,Chengdu University of Technology,Chengdu,Sichuan 610059;2) Ministry of Land and Resources Key Laboratory of Structure and Metallogenic Accumulation,Chengdu,Sichuan 610059;3) Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037;4) Hainan Institute of Geological Survey,Haikou,Hainan 570206;5) Sichuan Institute of Metallurgical and Exporation,Chengdu,Sichuan 610051;6) Anhui Institute of Geological Survey,Hefei,Anhui 230001 |
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| Abstract: | Based on reconnaissance survey and geological mapping as well as comprehensive literature review and laboratory study, this paper presents the following conclusions: Firstly, the Jiama-Kajunguo thrust-gliding nappe tectonic system, which resulted from the Indo-Asia collision, deformed successively from the central part of the basin toward the margin, the new layer overlay the old one, and the greatest deformation occurred around 50 Ma±. Secondly, the footwall block of the nappe is the Yeba group tectonite, the nappe consists of the upper Jurassic and lower Cretaceous carbonate and siliciclastics, the main part that is a complex fold with axial plane trends northward and can be divided into the fore-, mid- and post-parts from south to north structurally. The rock mass was located in the gliding nappe system at the top of the anticlinorium axis due to gravitational disequilibrium, which caused the hanging-wall block overlying the nappe to slip toward the north; the gliding nappe system is also divided into the fore-, mid- and post- parts from the south to the north in this paper. At last, the magmatic activities that induced the ore-forming alteration of the Jiama(Gyama) deposit happened during the releasing stage after the contraction stage of the thrust-gliding nappe tectonic system, and the upward migration of the magma was collaboratively controlled by the NS-trending basement faults and the thrusts. The magmatic rock that was emplaced finally in the fore-part of the thrust-gliding nappe tectonic system experienced multiple structural-magmatic-mineralization superimposition and generated the superlarge Jiama(Gyama) Cu polymetallic deposit. |
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| Keywords: | Jiama(Gyama)-Kajunguo thrust-gliding nappe tectonic system structural feature formation mechanism formation age factors controlling rocks and deposits |
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