摘要
新发现的低品位金矿与铜矿,主要类型浊积岩型、卡林型金矿和脉型与层控型铜矿,主要分布在紫阳—岚皋深大断裂和下古生代地层中。在适宜地质背景了解基础上,通过对含矿岩系,岩体与构造热液控矿特征和金、铜成矿条件分析,认为在安康地区金铜成矿条件是非常有利的。找金、铜前景是乐观的。
Low grade gold and copper deposits of new discoered. The mojor doposits types have turbity type-carlintyes types gold deposits and strata bound type-veintype capper deposits in both sides of feaft of lower palacozioic. This paper deals, with geological setting summasied ore-bering rock series. Cock body and tructure-hydrolhemal and gold and copper deposits of mineralization condition analysis so gold and copper prospecting in Ankang region is promising.
出处
《化工矿产地质》
CAS
2006年第2期87-93,共7页
Geology of Chemical Minerals
关键词
金-铜矿
断裂构造
下古生界
岩体(脉)
陕西安康地区
gold and copper, mineralization geology, minlization condition, Ankang region of Shaanxi
