摘要
红旗岭锡多金属矿床位于东坡矿田北东角,是千里山花岗岩岩体北侧的一个重要的矿床。该矿床赋存于震旦系下组浅变质砂岩中,受断裂裂隙控制,品位富,探明储量达6.3万t,属裂隙充填型(大型)高—中温热液矿床。
The Hongqiling Sn - polymetallic deposit is located at the northeastern comer of the Dongpo minefield and is an important deposit on the northern side of the Qianlishan granite mass. The deposit is confined to the Lower Sinian epimetamorphic sandstone and controlled by fracture and fissure and characterized by high- grade ore with reserves of 6.3 × 104 t Sn. The deposit is a high - meso- temperature hydrothermal filled deposit.
出处
《四川地质学报》
2007年第4期274-278,共5页
Acta Geologica Sichuan
关键词
矿床地质特征
矿床成因
锡多金属矿
湖南郴县红旗岭
geological feature of deposit
genesis of ores
Sn-polymetallic deposit
Hongqiling, Chenxian, Hunan
