Qitianling granite is a post-collisional , deep-sourced and hypabyssal, early Yanshanian high-K calc-alkaline granite complex pluton.
骑田岭花岗岩是燕山早期深源浅成的高钾钙碱性复式花岗岩岩体.
Qitianling pluton was formed by two phases emplacement and is mainly composed of early stage granite.
湘南骑田岭岩体主要由两阶段侵位所形成,早阶段侵位花岗岩组成骑田岭岩体的主体.
Structure features of the pluton and aureole rocks show that the emplacement of the stock was a diapiric process.
岩体和热变质岩的构造特征表明,该岩株是底辟作用侵位的产物。
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