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.
最引人注目的侵入体是岩脉。
层状侵入体与辉绿岩接触处有冷凝边，但都被岩脉所穿插。
The layered intrusions show chilled contacts against the diabases but are traversed by the dikes.
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