Within the belt ,the mid-late Proterozoic (epimetamorphic) green-schists were ovethrust from south to north onto the late Paleozoic granitic batholith at a low angle.

 
  • 中晚元古代淺變質(zhì)的綠片巖系自南向北以低角度輾掩于晚古生代花崗巖基之上。
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