摘要
水泄铜钴矿区地质条件较为复杂,控矿因素较多,通过分析认为主要受断层及岩性控制,地层初始富集,构造及区域变质作用提供通道及热源。水的循环、溶解作用形成热卤水成矿。
The geological conditions of Shuixie orefield are very complicated, with many ore control factors. According to the factor analysis, we think it is mainly controlled by the fault and lithological character, including the preliminary concentration in strata, channel and heat source provided by structure and regional metamprphism, deep circulation of water, hot brine formation by solution, etc.
出处
《云南地质》
2007年第4期416-420,共5页
Yunnan Geology
关键词
麦初菁组碎屑岩
N—E向断裂系
蚀变次生变富
铜钴矿
水泄永平云南
Clastic Rock of Maichuqing Formation
NE Fault System
Alteration SecondaryEnrichment
Cu- Co Deposit
Shuixie, Yongping
