摘要
柏杖子岩浆热液型金矿位于冀东~辽西贵金属矿化集中区东部,金矿体赋存于柏杖子岩体内及外接触带,柏杖子岩体为浅成~超浅成富含成矿元素及挥发份的同熔型花岗岩,成矿物质主要来源于柏杖子岩体,成矿岩石为富碱的酸性侵入岩,近矿围岩蚀变主要为硅化、钾化、绢云母化。
Baizhangzi which magma hot tybpe gold lie to east of the area that the east of Hebei to west of Liaoning noble metal mineralization centralize area.Gold-bed in the bedrock of baizhangzi and outside contact belt.The baizhangzi bed is hypabyssal exceed hypabyssal syntectite type granite,it is contain ore-forming element and volatilization rock.The ore-forming mostly root in baizhangzi rock-bed.The rock of ore-forming is contain alkaline acidity intrude rock.The rock round of ore-bed is eroded,the mostly reaso...
出处
《有色矿冶》
2005年第1期4-6,11,共4页
Non-Ferrous Mining and Metallurgy
关键词
柏杖子金矿床
地质特征
辽西
baizhangzi gold ore-bed
geology character: west of Liaoning