摘要
云南省漾濞县富恒金矿区褶皱、断裂构造极发育,化探Au-As-Hg-Sb综合异常强,浓集中心明显,并已圈定多个地表金矿(化)体吻合,成矿受岩性、构造破碎蚀变带控制,具微细浸染型金矿成矿特征。提出有利找矿地段为库木吾、岩前一带已知矿化体南北延伸方向及深部。
The Fuheng gold mine area, Yangbi County, Yunnan Province, has extremely developed fold and fracture structures, strong geochemical Au As Hg Sb comprehensive anomaly, obvious concentration center, multiple surface gold(geochemical) bodies have been delineated, and the mineralization is controlled by lithology and structural fracture alteration zone, with the characteristics of micro disseminated gold mineralization. It is proposed that the favorable prospecting area is the north-south extension direction and deep part of the known mineralized body in Kumuwu and Yanqian.
作者
孙贵荣
胡文奎
SUN Gui-rong;HU Wen-kui(Dali Institute of Yunnan Institute of Geology and Mineral Exploration,Dali 671000,China)
出处
《世界有色金属》
2022年第20期86-88,共3页
World Nonferrous Metals
关键词
云南省漾濞县富恒金矿
地质特征
找矿方向
Fuheng Gold Mine
Yangbi County
Yunnan Province
Geological characteristics
Prospecting direction