The research results indicate that the studied granites belong to A2-type which formed in late oro-genic extension environment and intruded in the process of the lithospheric delamination.
研究表明，花岗岩属A_2型，形成于造山晚期相对稳定的拉张环境，是在岩石圈拆沉过程中侵位的。
The research results indicate that the studied granites belong to A2-type which formed in late oro-genic extension environment and intruded in the process of the lithospheric delamination.
研究表明，花岗岩属A_2型，形成于造山晚期相对稳定的拉张环境，是在岩石圈拆沉过程中侵位的。
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