The synsedimentary deformation structures are common in eolian dunes, such as brecciated foresets, drag folds and overturned folds.

 
  • 見(jiàn)角礫化前積層、牽引褶曲、倒轉褶曲等常見(jiàn)的風(fēng)成沙丘同沉積變形構造。
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