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.
构造破碎带的石具有明显的对称分带性:破碎带的中心
钠柱石
,
两侧依次
榍石透辉石长英
带、黑云母钠长
带,并逐渐过
。钠柱石
的成因类型
沿构造破碎带产出的热液交代脉型。