The book is more satisfying if you read each chapter in sequence.
这本书依次读各章会更好。
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矿体,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。钠柱石矿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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