出露地层为震旦系、泥盆系、二叠系、三叠系以及侵入的花岗岩脉和花岗伟晶岩脉。
Emergence stratums are of Sinian, Devonian, Permian, Trias and intrusive granite dike and coarse - grained granite dike.
最引人注目的侵入体是岩脉。
岩脉山周围的岩脉与岩脉侵入时就已存在的放射状应力图像是相应的。
The Dikes surrounding dike Mountain parallel a radial stress pattern that existed at the time the dikes were intruded.
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