These siliciclastic rocks were derived mainly from the Archean and minor from Paleoproterozoic in the southern margin of the North China craton.

 
  • 源巖以太古宙地層為主,可能有古元古代地層的加入,經(jīng)歷了中等程度的風(fēng)化作用,并快速堆積形成的。
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