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.

构造破碎带的岩具有明显的带性：破碎带的中心为钠体，向两侧依次为榍辉长英岩带、黑云母钠长岩带，并逐渐过渡为围岩。钠的成因类型为沿构造破碎带产出的热液交代脉型。

The extrusive rock unit includes basalt, andesite, boninite and albitite as well as breccia and tuff.

喷出岩单元不仅仅由玄武岩组成，还包括安山岩、玻安岩、钠长岩以及角砾岩、凝灰岩等。