摘要
汉阴县铁佛—汉滨区流芳金矿带赋存于下志留统梅子垭组浅变质泥质碎屑岩中,其金矿化与区域性韧性剪切带及围岩蚀变密切相关,受层位、岩性和构造控制。
The gold mineralization zone lies in the Liufang area of the Tiefo-Hanbin district in Hanyin County, which occurs in slight metamorphosed pelitic clastics of the Meiyazi Formation of the Lower Silurian System. Gold mineralization in this area. has a close relation to the regionally ductile shearing zones and wall rock alteration and is confined by stratigraphy, lithology and structures.
出处
《陕西地质》
2010年第1期12-17,共6页
Geology of Shaanxi
基金
国土资源部矿产资源补偿费矿产勘查项目
任务书见国土资发[2003]422号文(2004年开展工作)
[2005〗249号文(2006年开展工作)
关键词
汉阴县铁佛-汉滨区流芳金矿
地质特征
找矿标志
the Liufang gold deposit in the Tiefo-Hanbin district of Hanyin county
geological features
ore prospecting indication
