The south margin faulted zone of Altun Mountain in Xinjiang is a regional upper mantle deep structure, along which numerous basic ultrabasiccomplex bodies are distributed.
阿尔金南缘断裂是一条深达上地幔的区域性大断裂，沿断裂分布着众多的基性-超基性杂岩体。
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The ultrabasic rocks form a complex of large tectonic slices with intercalated slices of Sebakwian sedimentary rocks.