会仙峰花岗岩体为燕山早期第三阶段侵入岩，是稀有元素矿化岩体，岩体蚀变具分带现象。

Huixianfeng granite body is a rare metal mineralized intrusive body of the third stage of early Yanshanian period with zoned alterations.

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第二发展阶段从燕山期以来，发展成为一条平移断裂带，属于狭义的环太平洋构造域的平移系统。

Second stage is a wrench fault system, which belongs to the Pacific Ocean cycle regime in narrow sense during the Yanshanian and Himalayan periods.

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有充分的证据表明，锡山花岗岩体是一个燕山晚期第二阶段两次侵入构成的复式岩体。

It has been fully shown from evidences that the granite body in Xishan is a complex body which was made up of two intrusions in the 2nd stage of Later Yenshanian period.

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