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.
构造破碎的岩石具有明显的对
性:破碎
的中心
钠柱石矿体,向两侧依次
榍石透辉石长英岩
、黑云母钠长岩
,并逐渐过渡
围岩。钠柱石矿的成因类
构造破碎
产出的热液交代脉
。