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岿美山钨矿床地质特征及其找矿标志
引用本文:邵海清,曾庆友,丁亮,范德友.岿美山钨矿床地质特征及其找矿标志[J].中国钨业,2013(6):13-16.
作者姓名:邵海清  曾庆友  丁亮  范德友
作者单位:[1]江西岿美山钨业有限公司,江西定南341902 [2]江西有色地质矿产勘查开发院,江西南昌330001 [3]江西稀有金属钨业控股集团,江西南昌330046
摘    要:岿美山钨矿位于南岭有色稀有金属成矿带的东端,其成矿地质条件优越,矿化分布普遍,具多种矿化类型,是赣南地区重要的找矿远景区。通过查阅以往岿美山钨矿成矿与找矿的成果资料,结合多年来从事钨矿勘查体会与实地工作经验,阐述了岿美山钨矿床的区域地质特征、矿区地层、构造、矿体特征、围岩蚀变和脉岩与钨的成矿关系,探讨了钨矿床的控矿因素、找矿标志,根据矿区钨矿脉的矿化信息、盲矿脉的产出规律及对应的成矿有利部位,提出矿区北东部为今后找矿、增储的重点区域。

关 键 词:钨矿床  地质特征  找矿标志  岿美山钨矿

Geological Characteristics and Prospecting Marks of Guimeishan Tungsten Deposit
Affiliation:SHAO Hai-qin, ZENG Qing-you2 (1. Jiangxi Guimeishan Tungsten Industry Co., Ltd., Dingnan 341902, Jiangxi, China; 2.Jiangxi Nonferrous Metal Geology and Mineral Resources Exploration and Exploitation Institute, Nanchang 330001, Jiangxi, China)
Abstract:Located in the eastern part of Nanling rare non-ferrous metals metallogenic belt, Guimeishan Tungsten Deposit, being an important prospecting region in Southern Jiangxi, enjoys favorable metallogenic geological conditions with diversified mineralization types. This paper studies the regional geological features, mine stratigraphy, structure, ore body characteristics, connection between rock alteration and dikes and tungsten mineralization of Guimeishan Tungsten Deposit based on retrieving the mineralization and prospecting documents combined with the author's tungsten prospecting field work. Ore-controlling factors, prospecting marks of the tungsten deposit are discussed. The analysis of mineralized veins information, output law of blind veins and corresponding favorable mineralized region reveals that the North-east part is the key potential prospecting and reserve-adding region.
Keywords:tungsten deposit  geological characteristics  prospecting marks
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