首页 | 本学科首页   官方微博 | 高级检索  
     检索      

阿舍勒铜锌块状硫化物矿床地质特征和成因
引用本文:叶庆同,傅旭杰,张晓华.阿舍勒铜锌块状硫化物矿床地质特征和成因[J].矿床地质,1997,16(2):97-106.
作者姓名:叶庆同  傅旭杰  张晓华
作者单位:[1]中国地质科学院矿床地质研究所 [2]中国地质科学院区划室
基金项目:“八五”国家科技攻关项目
摘    要:阿舍勒矿床与早-中泥盆世双峰式火山活动有着成因联系,产于火山洼地中,它在喷气-沉积阶段形成,后又细历了变质改造和岩浆热液叠加。矿床具有双层结构,很好的矿化分带和刨变分带。成矿流体的温度,压力和酸碱度等物理化学条件变化引起了围岩蚀变和矿石堆积,在海底界面上下形成了具有成因联系的两套矿化。

关 键 词:铜矿床  锌矿床  硫化物矿床  地质特征  成因

Geological Characteristics and Genesis of the Ashele Copper-zinc Massive Sulfide Deposit, Xinjiang
Ye Qingtong,Fu Xijie.Geological Characteristics and Genesis of the Ashele Copper-zinc Massive Sulfide Deposit, Xinjiang[J].Mineral Deposits,1997,16(2):97-106.
Authors:Ye Qingtong  Fu Xijie
Abstract:The Ashele massive sulfide deposit occurs in the Ashele Devonian volcano-sedimentary basin lying on the southern margin of Altay orogenic belt. The basin was formed as a result of rift evolution on the basis of Proterozoic-Early Paleozoic continental crust, and experienced deformation of regional nappe structure. Mineralization took place at the interval between Early-Middle Devonian volcanic activities of the bimocial spilite-keratophyre volcanic suite. The deposit has two-layer structure: a massive sulfide orebody in the upper part and a disseminated sulfide orebody in the lower part. In the massive sulfide orebody there exisths vertical zonation of S-Cu, S-Cu, Zn, S-Cu, Pb, Zn-Cu, Zn, Pb, BaSO4 which is a reflection of ore accumulation sequence at the bottom of the sea. Around the disseminated sulfide orebody are well-developed wall rock alterations, which exhibit from the inside outward the zonation of sericite-quartz metasomatite chlorite-sericite metasomatite weakly hydrolytic pyroclastic rocks, suggesting characteristics of acid leaching. Studies of ore deposit geology, temperature-pressture geochemistry and stable isotope geochemistry indicate that the ore-forming fluids were composed of deeply-circulating sea water and magmatic water, and that the ore-forming materials were derived from the lower crust. ln addition, the ore-forming process has been discussed and a metallogenic model of mixed fluids comprising deeply circulating sea water and magmatic water has been established.
Keywords:massive sulfide deposit  mineralization zoning  alteration zoning  metallogenic model  Ashele of Xinjiang  
本文献已被 CNKI 维普 等数据库收录!
点击此处可从《矿床地质》浏览原始摘要信息
点击此处可从《矿床地质》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号