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.
构造石具有明
称分
性:
中心为钠柱石矿体,向两侧依次为榍石透辉石长英
、黑云母钠长
,并逐渐过渡为围
。钠柱石矿
成因类型为沿构造
产出
热液交代脉型。