marialite

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.

构造破碎的岩具有明显的对称分性：破碎的中心钠柱矿体，向两侧依透辉长英岩、母钠长岩，并逐渐过渡围岩。钠柱矿的成因类型沿构造破碎产出的热液交代脉型。