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.

构造破具有明显对称分性：破中心为钠柱矿体，向两侧依次为榍透辉英、黑云母钠，并逐渐过渡为围。钠柱矿成因类型为沿构造破产出热液交代脉型。