marialite

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.

构造的岩具有明显的对称分性：的中心为矿体，向两侧依次为榍透辉长英岩、黑云母长岩，并逐渐过渡为围岩。矿的成因类型为沿构造产出的热液交代脉型。