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新疆萨吾尔山阔尔真阔腊金矿区的深部找铜研究

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新疆萨吾尔山阔尔真阔腊金矿区的深部找铜研究

尹意求;陈大经;唐红松;李嘉兴;胡兴坪;郭正林

【期刊名称】《桂林理工大学学报》 【年(卷),期】2001(021)002

【摘要】阔尔真阔腊地区位于新疆准噶尔西北缘萨吾尔山东部,为晚古生代岛弧构造环境,中性、中酸性火山-次火山岩浆活动频繁而强烈,火山角砾岩、隐爆角砾岩及火山机构十分发育,对次火山岩型铜(钴)成矿有利。阔尔真阔腊金矿与福建紫金山、台湾金瓜石铜金矿均属于酸性硫酸盐型浅成低温热液矿床,矿化蚀变特征极为相似。研究表明阔尔真阔腊金矿深部具有形成铜矿体的地质条件和找矿前景。%The Kuoerzhenkuola district is located in the easternSawuershan,the west-northern margin of the Zhungaer Basin,Xinjiang.The mineralizing environment was the island arc of the late Palaeozoic Era.The intermediate,intermediate-acidic volcanic-subvolcanic magmatism was frequent and strong.The volcanic breccia,cryptoexplosion breccia and volcanic apparatus very grew,which were favourable to the subvolcanic rock-type copper(cobalt) mineralization.The Kuoerzhenkuola gold deposit,Fujian Zijinshan and Taiwan Jinguashi copper-gold deposits all belong to the acidic sulfate type epithemal deposits,and the geological characteristics of the mineralization and the alteration also are similar.The study indicates that there are the geological conditions,which were formed the copper deposit, in the deep position of the Kuoerzhenkuola gold deposit,and

新疆萨吾尔山阔尔真阔腊金矿区的深部找铜研究

新疆萨吾尔山阔尔真阔腊金矿区的深部找铜研究尹意求;陈大经;唐红松;李嘉兴;胡兴坪;郭正林【期刊名称】《桂林理工大学学报》【年(卷),期】2001(021)002【摘要】阔尔真阔腊地区位于新疆准噶尔西北缘萨吾尔山东部,为晚古生代岛弧构造环境,中性、中酸性火山-次火山岩浆活动频繁而强烈,火山角砾岩、隐爆角砾岩及火山机构十分发育,对次
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