具“S”型花岗岩的特征，互相呈脉动侵入接触关系，形成于板内同造山期的环境。
It has features of "s" granite and as pulsation intrusion contact and formed the intraplate synorogenic period setting.
具“S”型花岗岩的特征，互相呈脉动侵入接触关系，形成于板内同造山期的环境。
It has features of "s" granite and as pulsation intrusion contact and formed the intraplate synorogenic period setting.
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