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.

构造破石具有明显对称分性：破中心钠柱石矿体，向两侧依次榍石透辉石英、黑云母钠，并逐渐过渡围。钠柱石矿成因类型沿构造破产出热液交代脉型。

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

主要组成矿物硬玉、霓辉石、镁纳闪石、蓝透闪石、镁角闪石、阳起石、石英、钠石、金红石和榍石。