江西大余西华山岩体边部找矿前景探讨  

The Rock Edge Exploration Potential in Xihuashan Tungsten Mine

作　　者：谢明璜[1] 王定生[1] 刘方[1] 彭杰[1] 陈瑞源[1] 

机构地区：[1]江西有色地质勘查二队,江西赣州341000

出　　处：《中国钨业》2013年第3期1-6,共6页China Tungsten Industry

基　　金：国家重点基础研究发展计划(973计划)项目(2007CB411404);国家自然科学基金资助项目(41073035)

摘　　要：西华山钨矿田成矿受复式花岗岩控制,含黑钨矿石英脉赋存于成矿花岗岩顶面原生裂隙带,称"西瓜皮"矿化。在总结西华山岩体地质与成矿特征的基础上,依据钨成矿与花岗岩体的关系,以及地表标志带特征及其分布,认为西华山岩体西侧、北侧和F1南东盘隐伏花岗岩顶部具有良好的找矿前景。The mineralization of Xihuashan Tungsten Mine is dominated by composite granite. Quartz veins containing wolframite are associated in the native fractured zone of top mineralized granite. This paper studies the relationship of tungsten mineralization and granite, and distribution of surface characteristics and based on the West HuaShan rock geology and mineralization characteristics. The results show that the northern side and F1 southeastern wall have favorable prospecting potential. marking western tape side,

关 键 词：隐伏花岗岩 内接触带 盲脉 钨矿床 

分 类 号：P612[天文地球—矿床学]