They can be divided into low sulphidation and high sulphidation types,with typical wall rock altera tion and alteration zonation of epit hermal de-posit.
这
矿床可分为高硫化型和低硫化型,且都具有典型的围岩蚀变、蚀变分带等矿床
。
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
造破碎带产出的热液交代脉型。
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