The main ore-bearing country rocks are aregillaceous limestone and marmarization limestone of upper-middle Cambrian.
其中寒武系上、中统大理岩化灰岩、泥质灰岩为主要含矿围岩。
There is an obvious rock zonation from the middle to bothsides of the structural shatter zone, generally from marialite orebody through diopside-felsite,biotite-albitite to the host Proterozoic rocks.
构造破碎带的岩石具有明显的对称分带:破碎带的中心为钠柱石矿体,向两侧依次为榍石透辉石长英岩带、黑云母钠长岩带,并逐渐过渡为围岩。钠柱石矿的成因类
为沿构造破碎带产出的热液交代脉
。
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