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.

构造破碎的石具有明显的对称分性：破碎的中心钠柱石矿体，向两侧榍石透辉石长英、黑云母钠长，渐过渡围。钠柱石矿的成因类型沿构造破碎产出的热液交代脉型。