Mineral constituents consist mainly of jadeite, aegirine-augite, magnesio-riebeckite, winchite, magnesio-hornblende, actinolite, quartz, albite, rutile and sphene.

主要组成矿物硬、石、镁纳闪石、蓝透闪石、镁角闪石、阳起石、石英、钠长石、金红石榍石。

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.

构造破碎带的岩石具有明显的对称分带性：破碎带的钠柱石矿体，向两侧依次榍石透石长英岩带、黑云母钠长岩带，并逐渐过渡围岩。钠柱石矿的成因类型沿构造破碎带产出的热液交代脉型。