However, the west and east margins of the Ordos Basin experienced distinct vertical movements, with the east margin uplifting and the west margin subsiding.

 
  • 至中生代燕山期,盆地受到了東西向擠壓作用,基底內部形態(tài)基本保持不變,盆地基底邊緣有明顯的垂向活動(dòng),具體表現為東升西降;
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