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哈萨克斯坦科翁腊德斑岩型铜矿地质特征与成矿模式
引用本文:韩淑琴,陈宣华,杨农,陈正乐,施炜,叶宝莹.哈萨克斯坦科翁腊德斑岩型铜矿地质特征与成矿模式[J].地质力学学报,2010,16(2):203-212.
作者姓名:韩淑琴  陈宣华  杨农  陈正乐  施炜  叶宝莹
作者单位:[1]中国地质科学院地质力学研究所,北京100081 [2]中国地质大学(北京),北京100083
基金项目:国家科技支撑计划重点项目
摘    要:哈萨克斯坦巴尔喀什成矿带科翁腊德斑岩型铜矿床从发现至今已经走过了70年的历程,它是发育在陆缘弧环境的典型超大型斑岩型矿床,具有花岗闪长岩型斑岩铜矿成因模式。矿床围岩蚀变与矿石矿物组合的垂直和水平分带明显,氧化带和次生硫化物富集带矿石品位高,易开采。矿床整体属于浅部成矿,受环状构造控制,次生石英岩和泥化等蚀变与矿床的关系最为密切。目前该矿床已开发殆尽,前景堪忧。

关 键 词:科翁腊德  斑岩型铜矿床  地质特征  成因模式  开发前景
收稿时间:2010/5/20 0:00:00

GEOLOGICAL CHARACTERISTICS AND METALLOGENIC MODEL OF SUPER-LARGE KOUNRAD PORPHYRY COPPER DEPOSIT, KAZAKHSTAN
HAN Shuqin,CHEN Xuanhu,YANG Nong,CHEN Zhengle,SHI Wei and Ye Baoying.GEOLOGICAL CHARACTERISTICS AND METALLOGENIC MODEL OF SUPER-LARGE KOUNRAD PORPHYRY COPPER DEPOSIT, KAZAKHSTAN[J].Journal of Geomechanics,2010,16(2):203-212.
Authors:HAN Shuqin  CHEN Xuanhu  YANG Nong  CHEN Zhengle  SHI Wei and Ye Baoying
Affiliation:1.Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijijng 100081,China;2.China University of Geosciences,Beijing 100083,China)
Abstract:The Kounrad porphyry copper deposit was discovered 70 years ago in the Balkhash Metallogenic Belt of the Central Asian Metallogenic Domain,.It is a typical super-large porphyry copper deposit developed under the tectonic environment of continental margin arc,with a metallogenic model of granodiorite.The vertical and lateral zonings of the wall rock alteration and ore mineral assemblages are obviously observed in the deposit.High content ore in the leaching zone and the ore deposition at a very shallow depth made it easy to be mined.It is suggested that the metallogenesis of the deposit was controlled by the circular structure,and had a very close relation with the secondary quartzite and argillic alteration.
Keywords:Kounrad  porphyry copper deposit  geological characteristics  metallogenic model  developing future
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