The orebody take the shape of prolate lenticle and appearing horizontal bedding.
区内有优质的硅藻土及硅藻粘土两个品级石。
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.
构造破碎带的岩石具有明显的对称分带性:破碎带的中心为钠柱石,向两侧依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。钠柱石的成因类型为沿构造破碎带产出的热液交代脉型。
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