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.
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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.
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