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.

构造破碎的石具有的对称分性：破碎的中心为钠柱石矿体，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。钠柱石矿的成因类型为沿构造破碎的热液交代脉型。

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.

构造破碎带具有明显对称分带性：破碎带钠柱体，向两侧依次榍透辉长英带、黑云母钠长带，并逐渐过渡围。钠柱成因类型沿构造破碎带产出热液交代脉型。

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.

构造破碎的石具有明显的对称分性：破碎的中心为钠柱石矿体，向两侧依次为榍石透辉石英、云母钠，并逐渐过渡为围。钠柱石矿的成因类型为沿构造破碎产出的热液交代脉型。

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.

构造破碎带的石具有明显的对称分带：破碎带的中心为钠柱石矿体，向两侧依次为榍石透辉石长英带、黑云母钠长带，并逐渐过渡为围。钠柱石矿的成因类型为沿构造破碎带产出的热液交代脉型。

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.

构造破碎带的具有明显的对称分带性：破碎带的中心为柱矿体，向两侧依次为榍英带、黑云带，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。

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.

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

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.

构带石具有明显分带性：带中心为钠柱石矿体，向两侧依次为榍石透辉石长英带、黑云母钠长带，并逐渐过渡为围。钠柱石矿成因类型为沿构带产出热液交代脉型。

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.

构造破碎带有明显对称分带性：破碎带中心为钠柱矿体，向两侧依次为榍透辉长英带、黑云母钠长带，并逐渐过渡为围。钠柱矿成因类型为沿构造破碎带产出交代脉型。

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.

构造破碎带石有显对称分带性：破碎带中心为钠柱石矿体，向两侧依次为榍石透辉石长英带、黑云母钠长带，并逐渐过渡为围。钠柱石矿成因类型为沿构造破碎带热液交代脉型。