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.
构造破碎带岩
具有明显
对称分带性:破碎带
中心为
体,向两侧依次为榍
透辉
长英岩带、
云母
长岩带,并逐渐过渡为围岩。
因类型为沿构造破碎带产出
热液交代脉型。