地质找矿论丛2012，Vol.27Issue(2)：156-161,6.DOI:10.6053/j.issn.1001-1412.2012.02.003
湘西南铜山岭地区钨多金属矿床地质特征及成矿机制探讨——以祥霖铺矿床为例
The geological features and minerogenetic mechanism of tungsten-polymetallic deposits in Tongshanling area,Southwestern Hunan: taking Xianglinpu deposit as an example
摘要
Abstract
Xianglinpu tungsten-polymetallic deposit is a skarn type ore deposit located at intersection of NE, NW and EW faults in the middle of Nanling latitudinal tectonic belt and mineraization concentrated a-bout the plunging crown of anticline. Studies on geological and geophysical and geochemical features of the deposit reveal that magmatism caused by Yanshanian tectonic movement supplied the heat source, fractures the channel-way and Qiziqiao formation of Middle Carbonferous Series the ore-forming materials. In the process of skarn metallization formed different mineral assemblages by which two metallogenic epoches and four metallogenic stages are recognized. Blind ore bodies are predicted in the west of the working area.关键词
祥霖铺钨多金属矿/矿床地质特征/成矿机制/湘西南地区Key words
Xianglinpu tungsten-polymetallic ore/ geological feature of the ore deposit/ minerogenetic mechanism/ southwest Hunnan province分类
天文与地球科学引用本文复制引用
杨冲,申志军,匡文龙,张万虎..湘西南铜山岭地区钨多金属矿床地质特征及成矿机制探讨——以祥霖铺矿床为例[J].地质找矿论丛,2012,27(2):156-161,6.基金项目
国家"高等学校特色专业建设点"项目(编号:TS11027)和湖南省国土资源厅软科学计划项目"郴州—炎陵断裂构造带W-Sn富集机理及找矿方向研究"(编号:2010-02)联合资助. （编号:TS11027）
