滑石片岩
After synsedimentary deposition, talc ores have also underwent strong metamorphism and deformation, which formed talc schist with typical schistosity structure.
滑石矿在经历了同生沉积-热液期之后,又受到了后期强烈的变质变形作用的叠加,形成了具片理构造的滑石片岩。
The talc-schist, talcmarble and biotite-schist are the most favourable hosting rocks to mineralization.
最有利于矿化的围岩是富镁的滑石片岩 、 含 滑石片 岩、含滑石大理岩和黑云母片岩等.
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