钠云母

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.

构造碎的石具有明显的对称分：碎的中心钠柱石矿体，向两侧依次榍石透辉石长英、黑云母钠长，并逐渐过渡围。钠柱石矿的成因类构造碎产出的热液交代脉。