Huixianfeng granite body is a rare metal mineralized intrusive body of the third stage of early Yanshanian period with zoned alterations.
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。
The viscoelastic parameter identification and back analysis are carried out by using the multi-stage loading creep curves of granite and schist .
在此基础上，针对花岗岩及片岩两种岩石的室内蠕变分级加载试验曲线进行了流变参数的识别与反演。
The metallogenic rock are biotite and intense-silicified granite-porphyry of the early stage of Xishan .
喜山早期黑云母花岗斑岩、强硅化花岗斑岩是区内斑岩型铜、钼矿床的成矿母岩。
The deposit belongs to the porphyry type molybdenum-mesothermal to epithermal lead and zinc deposit associated with the Xiaodonggou granite in late stage of Early Yanshan period.
矿床属于与燕山早期晚阶段小东沟花岗岩体有关的斑岩型钼矿床—中低温铅锌矿床。
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.
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.
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。
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