The Aksay and Subei basins are adjacent to Altyn Tagh fault system formed in Miocene and were considered as one basin cut by Altyn Tagh fault system in late Miocene.

 
  • 摘要阿克塞盆地和肅北盆地分列于阿爾金斷裂兩側,形成于中新世,有人認為它們曾是統一的盆地,在中新世末期由于阿爾金斷裂的活動(dòng)而被分割。
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