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

主要组成硬玉、霓辉、镁纳闪、蓝透闪、镁角闪、阳起、英、钠长、金红榍。

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对称分带性：破碎带的中心钠体，向两侧依次榍透辉长英岩带、黑云母钠长岩带，并逐渐过渡围岩。钠的成因类型沿构造破碎带产出的热液交代脉型。