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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第43卷

期数:

2021年第01期

页码:

12-35

栏目:

基础地质与矿产地质

出版日期:

2021-01-15

文章信息/Info

Title:

Ore-forming System and Regularity of Important Metallogenetic Belts in East Tianshan, China

作者:

张连昌¹; 2; 3; 董志国¹; 2; 3; 陈 博⁴; 张 新¹; 2; 3; 张帮禄¹; 2; 朱明田¹; 2; 3; 计文化⁴; 冯 京⁵

(1. 中国科学院地质与地球物理研究所 中国科学院矿产资源研究重点实验室,北京 100029; 2. 中国科学院地球科学研究院,北京 100029; 3. 中国科学院大学 地球与行星科学学院,北京 100049; 4. 中国地质调查局西安地质调查中心,陕西 西安 710054; 5. 新疆维吾尔自治区地质矿产勘查开发局,新疆 乌鲁木齐 830000)

Author(s):

ZHANG Lian-chang¹; 2; 3;  DONG Zhi-guo¹; 2; 3;  CHEN Bo⁴;  ZHANG Xin¹; 2; 3;  ZHANG Bang-lu¹; 2;  ZHU Ming-tian¹; 2; 3;  JI Wen-hua⁴;  FENG Jing⁵

(1. Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; 2. Innovation Academy of Earth Science, Chinese Academy of Sciences, Beijing 100029, China; 3. College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China; 4. Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, Shaanxi, China; 5. Xinjiang Bureau of Geo-exploration and Mineral Development, Urumqi 830000, Xinjiang, China)

关键词:

成矿区带;  成矿系统;  成矿规律;  构造演化;  斑岩型铜矿床;  古生代;  东天山;  中亚造山带

Keywords:

Key words: metallogenic belt;  ore-forming system;  metallogenic regularity;  tectonic evolution;  porphyry Cu deposit;  Paleozoic;  East Tianshan;  Central Asian orogenic belt

分类号:

P612

DOI:

10.19814/j.jese.2020.10025

文献标志码:

A

摘要:

成矿区带一般指具有矿产资源潜力的成矿地质单元,而成矿系统主要从成矿要素、成矿作用过程角度研究成矿的总体特征,包括矿床组合、成矿系列及其联系,是划分成矿区带及总结成矿规律的重要依据。东天山造山带位于吐哈盆地与塔里木地块之间,可划分为大南湖—头苏泉铜金多金属成矿带、康古尔塔格—黄山金铜镍成矿带、阿齐山—雅满苏铁铜多金属成矿带及彩霞山—吉源铅锌银多金属成矿带。东天山构造演化与成矿具有明显的多阶段性,并形成多个成矿系统:①中—晚元古代古陆缘伸展环境形成铅锌银沉积矿床成矿系统; ②奥陶纪—石炭纪活动大陆边缘环境形成VMS型铜锌矿床和斑岩型铜矿床成矿系统; ③石炭纪岛弧环境形成火山岩型铁铜矿床成矿系统; ④晚石炭世—早二叠世后碰撞造山及地幔柱叠加阶段,形成岩浆型铜镍矿床成矿系统和与剪切活动有关的金矿床成矿系统。

Abstract:

The metallogenic belt is a geological unit for possessing potential of ore resources. The metallogenic system mainly focuses on the overall characteristics of mineralization from the aspects of metallogenic elements and processes, including deposit assembly, metallogenic series and their original link. The metallogenic system is an important evidence for dividing metallogenic belt and summarizing metallogenic regularity. East Tianshan orogenic belt, which is sandwiched between Tuha Basin and Tarim block, may be divided into four metallogenic belts in terms of spatial distribution, including Dananhu-Tousuquan Cu-Au-polymetallic metallogenic belt, Kanggurtag-Huangshan Au-Cu-Ni metallogenic belt, Aqishan-Yamansu Fe-Cu-polymetallic metallogenic belt and Caixiashan-Jiyuan Pb-Zn-Ag-polymetallic metallogenic belt. The temporal evolution of East Tianshan orogenic belt is distinctly characterized by multi-stage and multiple metallogenic system, including ① Middle-Late Proterozoic extension continental margin, where there occurs a metallogenic system of sedimentation Pb-Zn-Ag deposits; ② Ordovician-Carboniferous active continental margin, where there occurs a metallogenic system of VMS Cu-Zn deposits and porphyry Cu deposits; ③ Carboniferous island arc, where there occurs a metallogenic system of volcanic Fe-Cu deposits; ④ Late Carboniferous-Early Permian post-collision orogeny and superimposition of mantle plume, where there occurs a metallogenic system of magmatic Cu-Ni deposits and a metallogenic system of Au deposits related to ductile shear processes.

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备注/Memo

备注/Memo:

收稿日期:2020-10-18; 修回日期:2020-11-10投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家重点研发计划项目(2018YFC0604001); 国家自然科学基金项目(U1703242)
作者简介:张连昌(1959-),男,陕西西安人,中国科学院地质与地球物理研究所研究员,博士研究生导师,理学博士,1979～1983年在西安地质学院(现长安大学)地质勘查专业攻读学士学位,1985～1988年在成都地质学院和西安地质学院(联合培养)矿床学专业攻读硕士学位,1988～2000年在长安大学(原西安地质学院、西安工程学院)先后任讲师、副教授,E-mail:lczhang@mail.iggcas.ac.cn。

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