Otherwise with Paleotethys closing in late Triassic period,the pull-apart continental margin reversed in Indo-China movement creating Indo-Chinafolded orogeny.

 
  • 晚三疊紀隨古特提斯的閉合,經(jīng)印支運動(dòng)張裂陸緣發(fā)生反轉,形成印支褶皺造山帶。
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