felsite

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.

碎带岩石具有明显对称分带性：碎带中心为钠柱石矿体，向两侧次为榍石透辉石长英岩带、黑云母钠长岩带，并逐渐过渡为围岩。钠柱石矿类型为沿碎带产出热液交代脉型。