1.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.

1.构造破碎带的有明显的对称分带性：破碎带的中心为柱矿体，向两侧依次为榍透辉长英带、黑长带，并逐渐过渡为围。柱矿的成因类型为沿构造破碎带产出的热液交代脉型。