Central Orogenic System 中央造山系
Kazakhstan tien shan orogenic system 天山造山系
nonplate-collision orogenic system 非板块碰撞造山体制
As major parts of the central orogenic system, the Qinling and Kunlun orogens constitute a giant orogenic belt that stretches from east to west in central China.
秦岭、昆仑造山带是中央造山系的主要组成部分，东西连接构成一条东西横贯我国大陆中部的巨型造山带，它不论是对中国大陆构造基本格局的形成还是对现今中国南北近地表系统的差异均具有十分重要的影响。
参考来源 - 西秦岭—东昆仑造山带的衔接转换与共和坳拉谷·2,447,543篇论文数据，部分数据来源于NoteExpress
Petroleum geological condition in the south edge of central orogenic system is fairly favorable but the cur- rent exploration level is low.
中央造山系南缘油气地质条件比较优越，然而勘探程度较低。
The residual basins were deeply buried in Himalayan Period, and the Carboniferous System was piecemeal distributed in the depressed belts of orogenic zone.
喜山期残存盆地深埋，石炭系仅零星残存在造山带的低洼地带。
Sedimentary basin and adjacent orogenic belt are two basic tectonic units of continent and twins developed in a geodynamic system.
毗邻的沉积盆地与造山带是大陆构造的基本单元和形成于统一地球动力学系统中的一对孪生体。
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