It trends nearly E-W and is a dissymmetrical anticline belt with steep dip angle in the north limb and gentle in the south.

 
  • 該構造帶走向近東西,為北陡南緩兩翼不對稱(chēng)的隆起帶,上部發(fā)育“塌陷式”地塹斷裂系統。
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