We suggest that the strata are turbidite sequences that are deposisted on the passive continental margin.The strata containing plant, conodont and graptolite belongs to Early-Late Devonian.

 
  • 該組中采獲了低等蕨類(lèi)植物、牙形石和筆石等化石,證實(shí)其時(shí)代屬于早泥盆世-晚泥盆世。
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