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.

构造破碎的石具有明显的对称分性：破碎的中心钠柱石矿体，向两侧依石透辉石长英、黑云母钠长，逐渐过渡围。钠柱石矿的成因类型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.

构造破碎的具有明显的对称分性：破碎的中心钠柱矿体，向两侧依次透辉英、黑云母钠，并逐渐过渡围。钠柱矿的成因类型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.

造破碎的石具有明显的对称：破碎的中心钠柱石矿体，向两侧依次榍石透辉石长英、黑云母钠长，并逐渐过渡围。钠柱石矿的成因类型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.

构造破碎的石具有明显的对称分性：破碎的中心钠柱石矿体，向两侧榍石透辉石长英、黑云母钠长，渐过渡围。钠柱石矿的成因类型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性：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.

破碎的石具有明显的对性：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性：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。