A steep slope zone is recognized between the central uplift and the eastern depression and can be classified as a slope break zone resulted from the double action of tectonism and erosion.

 
  • 研究發(fā)現,在盆地中部隆起與東部坳陷之間存在著(zhù)一個(gè)陡坡帶,可將其歸為構造與侵蝕雙重作用成因的坡折帶。
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