According to field investigation,the Yingfeng rapakivi granite is formed in mid-Proterozoic and located between shear belts as a lentiform in the structural belt of north margin of Qaidam basin.

 
  • 野外調查表明,鷹峰環(huán)斑花崗巖體形成于中元古代,位于柴北緣構造帶,呈透鏡狀夾持在剪切帶間。
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