In the northwest Pacific domain, the folding age is from Late Jurassic to Middle Eocene, and in the Tethys domain it is between Middle and Late Eocene.

 
  • 主要褶皺時(shí)代很晚,在南北太平洋大地構造域是晚侏羅世至中始新世,在特提斯大地構造域是中晚始新世之交。
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