富蕴县结勒迪喀腊金矿成矿模式及找矿标志分析  

Fuyun County junction metallogenic model and prospecting gold Ledu Cameroon wax marker analysis

作　　者：胡万里 HU Wan-li(Fourth Geological Team of the Xinjiang Uygur Autonomous Region geological and mineral exploration and Development Bureau, Aletai 836500,China)

机构地区：[1]新疆维吾尔自治区地质矿产勘查开发局第四地质大队,新疆阿勒泰836500

出　　处：《世界有色金属》2018年第1期104-104,106,共2页World Nonferrous Metals

摘　　要：新疆北部阿勒泰成矿带的结勒迪喀腊金矿的发现引起了众多单位和学者的关注,带动了该区金、铜、铬、铁等多金属的研究和外围找矿工作。结勒迪喀腊金矿位于扎河坝-阿尔曼台金、铜、铬、铁等多金属成矿带中段,金矿体赋存于北西向构造蚀变带中,成矿地质条件非常有利。对该地金矿成矿地质特征、成矿规律进行分析和研究,该矿床浅成超浅成侵入体型金矿。The northern Xinjiang Aletai metallogenic belt knot Ledu Cameroon wax gold deposit was discovered by many units and the attention of scholars,led the research and the external area of gold and copper,chromium,iron and other metal ore prospecting work.Node Ledu Cameroon La zhaheba Arman Taiwan gold deposit is located in gold,copper,chromium,iron polymetallic metallogenic belt.The ore bodies occur in NW tectonic alteration zone,favourable metallogenic conditions.The metallogenic geological characteristics and metallogenic regularity of the gold deposit are analyzed and studied.The deposit is shallow and ultra shallow into the type of gold deposit.

关 键 词：阿勒泰成矿带 金矿床 地质特征 成矿模式 

分 类 号：P618.51[天文地球—矿床学]