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.

构造碎的岩具有明显的对称分：碎的中心为钠柱矿体，向两侧依次为辉长英岩、黑云母钠长岩，并逐渐过渡为围岩。钠柱矿的成因类型为沿构造碎产出的热液交代脉型。