中国及境外天山铅锌成矿作用与找矿方向  

Zn-Pb Metallogeny and Prospecting Orientation of Tianshan in China and Abroad

作　　者：高荣臻[1,2,3] 薛春纪 满荣浩[1,2] 代俊峰 赵晓波 赵云[1,2] 亚夏尔·亚力坤[5] Bakhtiar NURTAEV Nikolay PAK 莫宣学 GAO Rong-zhen;XUE Chun-ji;MAN Rong-hao;DAI Jun-feng;ZHAO Xiao-bo;ZHAO Yun;Yaxia er YALIKUN;Bakhtiar NURTAEV;Nikolay PAK;MO Xuan-xue(School of Earth Sciences and Resources,China University of Geosciences,Beijing 100083,China;State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Beijing 100083,China;School of Resources and Civil Engineering,Northeastern University,Shenyang 110819,Liaoning,China;School of Earth Sciences,East China University of Technology,Nanchang 330013,Jiangxi,China;School of Geology and Mining Engineering,Xinjiang University,Urumqi 830047,Xinjiang,China;Institute of Geology and Geophysics,State Committee of the Republic of Uzbekistan on Geology and Mineral Resources,Tashkent 100041,Uzbekistan;Institute of Geology,National Academy of Sciences of Kyrgyz Republic,Bishkek 720040,Kyrgyzstan)

机构地区：[1]中国地质大学(北京)地球科学与资源学院,北京100083 [2]中国地质大学(北京)地质过程与矿产资源国家重点实验室,北京100083 [3]东北大学资源与土木工程学院,辽宁沈阳110819 [4]东华理工大学地球科学学院,江西南昌330013 [5]新疆大学地质与矿业工程学院,新疆乌鲁木齐830047 [6]乌兹别克斯坦地质与矿产资源委员会地质与地球物理研究所,塔什干100041 [7]吉尔吉斯斯坦科学院地质研究所,比什凯克720040

出　　处：《地球科学与环境学报》2021年第1期36-79,共44页Journal of Earth Sciences and Environment

基　　金：国家重点研发计划“深地资源勘查开采”重点专项项目(2017YFC0601202);国家自然科学基金项目(41902067);“十二五”国家科技支撑计划项目(2011BAB06B02)。

摘　　要：中国及境外天山铅锌矿床多有发现,如哈萨克斯坦Tekeli、Shalkiya和Achisai,乌兹别克斯坦Kurgashinkan和Uchkulach,塔吉克斯坦Altyntopkan,中国新疆乌拉根、彩霞山、阿齐山、阿尔恰勒等大型—超大型铅锌矿床,构成了天山巨型铅锌成矿带。这些铅锌矿床形成于怎样的地球动力学背景?铅锌成矿的基本地质特征是什么?有哪些重要成矿类型?受何要素控制?未来找矿突破方向在哪里?这些都是颇受关注的地质找矿问题。在广泛矿产地质调查和综合分析前人研究成果的基础上,将中国及境外天山作为整体,综述了天山造山带构造演化和重要铅锌成矿环境、典型矿床特征与成矿系统/成矿类型,总结了天山地区铅锌成矿演化过程,并分析了区域铅锌成矿特点与找矿突破方向。结果表明:天山造山带经历了前寒武纪古陆形成、洋-陆俯冲增生、陆-陆碰撞造山和陆内成盆4个地球动力学过程,先后出现了元古宙古陆边缘裂陷盆地、古生代洋-陆俯冲增生岛弧、晚古生代陆-陆碰撞造山与中—新生代山前/山间盆地4类重要铅锌成矿环境。在元古宙古陆边缘裂陷盆地环境,主要受同生断层、还原性细碎屑岩-碳酸盐岩建造等控制,形成了古陆边缘裂陷盆地铅锌成矿系统与SEDEX型铅锌矿床;在古生代洋-陆俯冲增生岛弧环境,主要受弧岩浆活动、断裂构造、地层等控制,形成了增生岛弧铅锌成矿系统与矽卡岩型、斑岩型、岩浆热液脉型、VMS型铅锌矿床;在晚古生代陆-陆碰撞造山环境,主要受被动陆缘海相碳酸盐岩、张性开放空间、逆冲推覆构造等控制,形成了碰撞造山铅锌成矿系统与MVT型铅锌矿床;在中—新生代山前/山间盆地环境,主要受盆地三元结构、油气运移与红层“漂白”、硫酸盐岩等控制,形成了山前/山间盆地铅锌成矿系统与砂岩型铅锌矿床。由此可见,天山地区存在多种铅锌成矿环境和�There are many Zn-Pb deposits in Tianshan of China and abroad,forming a giant Zn-Pb metallogenic belt.Why so many Zn-Pb deposits are located here?how geodynamic setting results in their formation?What is the regional ore-forming types and the key to the Zn-Pb metallogeny?Where is the future prospecting orientation?All these significant geological and exploration problems are attracted much more attentions.Based on investigating the regional geology and Zn-Pb deposits in Tianshan and consulting various references,the important metallogenic environments,geological characteristics of typical Zn-Pb deposits and their ore-forming types were demonstrated,and tectonic-metallogenic evolution of Tianshan orogen and prospecting direction of Zn-Pb mineral resources were then discussed.The results show that Tianshan orogen experiences four geodynamic processes,namely the formation of Precambrian continent,ocean-continent subduction accretion,continent-continent collision orogeny,and intraplate deformation,and four corresponding metallogenic environments,including Proterozoic paleo-continent margin rift basin,Paleozoic ocean-continent subduction accretion island arc,Late Paleozoic continent-continent collision orogeny and Meso-Cenozoic depression basin.Accordingly,four important metallogenic systems and ore-forming types are formed as follow.The SEDEX Zn-Pb deposits are formed in Proterozoic paleo-continent margin rift basin environment,and controlled by contemporaneous faults and reduced fine-grained clastic rocks or carbonate rocks.The skarn,magmatic hydrothermal vein and VMS Zn-Pb deposits are formed in island arc of Paleozoic ocean-continent subduction accretion environment,and controlled by arc-related magmatism,faults and favorable strata.The MVT Zn-Pb deposits are formed in Late Paleozoic continent-continent collision orogeny environment,and controlled by marine carbonate in passive margin,extensional faults and thrust nappe structures.The sandstone-hosted Zn-Pb deposits are formed in Meso-Cenozoic depression basin env

关 键 词：铅锌矿床 成矿作用 成矿环境 成矿类型 控矿要素 成矿特点 找矿方向 天山 

分 类 号：P611[天文地球—矿床学] P612[天文地球—地质学]