东天山铜金多金属矿床成矿系统和成矿地球动力学模型

毛景文; 杨建民; 韩春明; 王志良

东天山铜金多金属矿床成矿系统和成矿地球动力学模型

毛景文^{1, 2,},
杨建民²,
韩春明^{1, 2},
王志良^{1, 2}

1.
中国地质大学地球科学与资源学院, 北京 100083
2.
中国地质科学院矿产资源研究所, 北京 100037

基金项目:

国家重点基础规划项目 G19990432016

国土资源部地质大调查项目 DKD99002001

详细信息

作者简介:
毛景文(1956-), 男, 研究员, 博士生导师, 从事矿床地质和地球化学研究. E-mail: jingwenmao@263.net

中图分类号: P618.41;P618.51;P611.5
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- 被引次数: 0
出版历程
- 收稿日期: 2001-11-12
- 刊出日期: 2002-07-25

Metallogenic Systems of Polymetallic Copper and Gold Deposits and Related Metallogenic Geodynamic Model in Eastern Tianshan, Xinjiang

1.
Faculty of Earth Sciences and Mineral Resources, China University of Geosciences, Beijing 100083, China
2.
Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037

摘要

摘要: 近年来, 在东天山地区地质找矿不断取得突破, 一系列大型、中型铜金矿床先后被发现.绝大多数铜金矿床在空间上密集分布于黄山-康古尔缝合-剪切带两侧的岛弧带内, 时间上集中在石炭纪—二叠纪.金矿床包括造山型、石英脉型和浅成低温热液型, 铜矿床包括斑岩型、夕卡岩型和热液脉型及铜镍硫化物型.金、铜和铜镍矿化各自成系统产出, 为板块俯冲晚期和碰撞期后大规模镁铁质-超镁铁质和中酸性-酸性花岗质岩浆侵位-喷发事件的产物.
- 金矿床 /
- 铜矿床 /
- 成矿系统 /
- 地球动力学 /
- 东天山
Abstract: In the past several years, a number of copper, gold and Cu Ag Pb Zn deposits have been discovered and explored in the eastern Tianshan area, Xinjiang. All of the metallic deposits are spatially and densely distributed within the Devonian Late Carboniferous island arc in the north and Carboniferous island arc in the south along the Kangguer Huangshan Carboniferous Permian suture large scale shear zone. These deposits, formed temporally in Carboniferous Permian, can be grouped into gold deposit system comprising epithermal, orogenic and quartz vein types, copper deposit system, porphyry, skarn and hydrothermal vein types, and Cu Ni sulfide system. The three metallogenic systems are genetically associated with the emplacements and eruptions of mafic ultramafic or intermediate felsic magmas during the subduction and extension of post collision of the plates.
- gold deposit /
- copper deposit /
- metallogenic sytem /
- geodynamics /
- eastern Tianshan

HTML全文

图 1 东天山大地构造单元与铜金矿床分布

基于杨兴科等^[9]和芮宗瑶等^[31]构造与成矿图基础上改编而成.根据芮宗瑶等^[34]和秦克章^④放射性同位素测年资料, 土屋-黄山岛弧形成于晚泥盆世; 李锦轶(与笔者讨论) 初步研究证明小热泉一带原下石炭统为泥盆纪的岩层; 因此都属于大南湖-头苏泉岛弧的一部分.1.小热泉子铜矿; 2.石英滩金矿; 3.康西金矿; 4.康古尔金矿; 5.马头滩金矿; 6.维权铜矿; 7.夹白山金矿; 8.延东铜矿; 9.土屋铜矿; 10.灵龙铜矿; 11.赤湖铜矿; 12.小红山金矿; 13.路白山铜矿; 14.土墩铜镍矿; 15.二红洼铜镍矿; 16.香山铜镍矿; 17.黄山铜镍矿; 18.黄山东铜镍矿; 19.148金矿; 20.梧桐窝子南金矿; 21.白石沟金矿

Fig. 1. Distribution of tectonic units and gold-copper deposits in eastern Tianshan

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图 2 东天山金矿成矿系统模式

Fig. 2. Metallogenic system model of gold deposits in eastern Tianshan

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图 3 东天山铜矿成矿系统模式

Fig. 3. Metallogenic system model of copper deposits in eastern Tianshan

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图 4 东天山晚古生代地球动力学演化与成矿模式

Fig. 4. Geodynamic evolution and metallogenic model of Late Paleozoic in eastern Tianshan

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