摘要
羊廷寺金红石矿床位于五台西段草垛山—分岭背斜南翼,金红石矿体赋存于碾子沟上段地层中,矿体产状与地层产状一致,矿化是吕梁期热液活动强烈影响的结果,矿床矿岩石主要为阳起透闪岩、绿泥透闪岩等。基性变质岩与后期构造热液活动叠加的地段是今后找矿方向。
Yangtingsi ruffle deposit is located in Huyu Town, Daixian County, Shanxi Province. The deposit is situated in the south wing of Caoduoshan anticline and ore bodies is distributed in the upper parts of Nianzigou for- mation. Occurrence of the ore bodies similar to that of strata. Rutile mineralization wag result of hydrothermal activities in the Luliang period. Ore-beating rocks in the deposit are mainly actinolite tremolite and chlorite tremolite. Basic metamorphic rocks and late hydrothermal activity superimposed tectonic lots are prospecting direction of the future.
出处
《太原科技》
2009年第8期71-72,77,共3页
Taiyuan Science and Technology
关键词
金红石矿床
地质特征
找矿方向
羊廷寺
rutile deposit
geological characteristics
prospecting direction
Yangtingsi
