The south margin faulted zone of Altun Mountain in Xinjiang is a regional upper mantle deep structure,along which numerous basic ultrabasic complex bodies are distributed.

 
  • 阿爾金南緣斷裂是一條深達上地幔的區域性大斷裂,沿斷裂分布著(zhù)眾多的基性-超基性雜巖體。
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