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.

构造的具有明显的对称分性：的中心为钠柱矿体，向两侧依次为榍透辉长英、黑云母钠长，逐渐过渡为围。钠柱矿的成因类型为沿构造产出的热液交代脉型。