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
的岩石具有明显的对称分性：的中心为钠柱石矿体，向两侧依次为榍石透辉石长英岩、黑云母钠长岩，并逐渐过渡为围岩。钠柱石矿的成因类型为沿构造产出的热
脉型。
表本软件的观点；若发现问题，欢迎向我们指正。
