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：破碎带的中心钠柱，向两侧依次榍透辉长英带、黑云母钠长带，并逐渐过渡。钠柱的成因类型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.

构造破碎带的石具有明显的对称分带性：破碎带的中心为钠柱石矿体，向两为榍石透辉石长英带、黑云母钠长带，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.

构造破碎带的石具有明显的对称分带性：破碎带的中心为钠柱石矿体，向次为榍石透辉石长英带、黑云母钠长带，并渡为围。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.

构造破石具有对称分性：破中心为钠柱石矿体，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。钠柱石矿成因类型为沿构造破出热液交代脉型。

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.

碎带的石具有显的对称分带性：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。钠柱石矿的成因类为沿碎带产出的热液交代脉。

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.

构造的石具有明显的对称分性：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。钠柱石矿的成因类为沿构造产出的热液交。