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珲春东部金铜钨矿带找矿地质条件及找矿方向
引用本文:王玉宝,韦鹏飞,时俊峰.珲春东部金铜钨矿带找矿地质条件及找矿方向[J].吉林地质,2009,28(3):35-38,46.
作者姓名:王玉宝  韦鹏飞  时俊峰
作者单位:吉林省有色金属地质勘查局603队,吉林,珲春,133300
摘    要:论述了珲春东部金铜钨矿带成矿地质条件,认为下古生界志留系下统五道沟群变质岩,印支—燕山期杂岩体是金铜钨的成矿主要矿源体;分析了典型矿床杨金沟白钨矿床的成因机制,确定为层控与岩浆热液复合型白钨矿床;指出成矿带下段找矿思路。

关 键 词:成矿地质条件  杨金沟钨矿床  找矿方向

Ore-forming geological conditions and prospecting direction of Au-Cu-W ore belt of eastern part of Hunchun, Jilin Province
WANG Yu-bao,WEI Peng-fei,SHI Jun-feng.Ore-forming geological conditions and prospecting direction of Au-Cu-W ore belt of eastern part of Hunchun, Jilin Province[J].Jilin Geology,2009,28(3):35-38,46.
Authors:WANG Yu-bao  WEI Peng-fei  SHI Jun-feng
Institution:(Team 603, Bureau of Nonferrous Metals Geological Prospecting of Jilin Province, Hunchun 133300, Jilin, China)
Abstract:The paper discussed the ore-forming geological conditions of Au-Cu-W ore belt of eastern part of Hunchun, it is considered that metamorphic rock of Wudaogou Group, lower Paleozoic Silurian period, Indo-Chinese- Yanshanian complex body is a main source rock of Au-Cu-W, meanwhile, analyzed the formation mechanism of Yangjingou scheelite deposit, which belongs to composite stratabound and magmatic hydrothermal scheelite deposit, and pointed out prospecting ideas in the lower of the metallogenic belt.
Keywords:ore-forming geological condition  Yangiingou scheelite deposit  prospecting direction
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