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)高一中温热液矿床。[著者文摘]
文章出处:
《四川地质学报》-2007年27卷4期 -274-278页
Acta Geologica Sichuan
栏目信息:
分 类 号:
文献标识码:
A
文章编号:
1006-0995(2007)04-0274-05
相关文章:
Geological Features and Genesis of the Hongqiling Sn- polymetallic Deposit in Chenxian, Hunan
SU Yong-mei (South Hunan Institute of Geological Exploration, Chenzhou, Hunan 423000)
Abstract:
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.[著者文摘]
Key words:
geological feature of deposit; genesis of ores; Sn-polymetallic deposit; Hongqiling, Chenxian, Hunan
收稿日期: 2007-07-05

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