摘要
永平大型铜硫(钨)矿床是江西北武夷铜多金属成矿带中的典型矿床之一,矿床受晚古生代盆地控制,在海西-印支期推覆构造的影响下,发育了一组北北东向的推覆断层,使基底周潭岩组(混合岩)超覆在石炭系藕塘底组地层之上。十字头岩体在矿层基本成型之后斜切矿层向上侵入,切割矿层及围岩,对原已成型的矿层起着叠加改造作用,其岩浆期后成矿热液本身存在着垂直矿化分带,在深部围绕十字头岩体外接触带的上盘存在进一步寻找隐伏盲矿体的找矿前景。
Yongping large - scale Cu - S（Tunsten） deposit is one of the typical deposits in the North Wuyi copper polymetal mineralization zone in Jiangxi. The deposit is controlled by late Paleozoic basin, it develops a goup of N - NE overturn faults under the influence of Haixi - Yinzhi overturn structure, to make the base Zhoutan rock group（ mixed rock） overlapped on the Carbonacous Outan bottom group. After a serious of acitivities, there is a great prospect of finding latent blind orebodies in the area.
出处
《铜业工程》
CAS
2009年第2期10-12,19,共4页
Copper Engineering
