Taihangshan orogen, called tectonomagmatic belt by most of geologists, is thought to be a part of Mesozoic circum Pacific magmatic arc.
太行山造山带被大多数学者称为构造岩浆带，被认为是中生代环太平洋岩浆弧的组成部分。
Being an important pluton in the western part of Altay orogen, Tielieke pluton shows arc granitoid characteristics.
铁列克岩体是阿尔泰造山带西段的一个重要的岩体，显示弧花岗岩特征，其侵位时代一直没有解决。
Lead isotope compositions of ore sulfides suggest multiple sources for the metals that range from the crust to the mantle, with certain amounts derived from the orogen or island arc.
铅同位素组成反映主要来源于造山带或成熟弧环境，上地壳铅也不同程度地提供了成矿物质。
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