The Qinling orogenic belt is the division of geology, geochemistry, physical geography and geography between north China and south China, so it has become the focus of many geologists of the world.
秦岭造山带横贯中国东部，是中国大陆南北地质、地球化学、地球物理以及自然地理的分界线，因此，一直受到国内外地质学者的极大关注。
参考来源 - 北秦岭（陕西段）古生代构造体制转换研究Qinling orogenics belts is is one of mountain ranges in China ,is the North China Plate and the Yangtze plate boundary.
秦岭造山带位于中国中央造山带体系，是我国重要的山脉之一，是华北板块与扬子板块的分界线。
参考来源 - 秦岭洛南—栾川断裂带运动学特征·2,447,543篇论文数据，部分数据来源于NoteExpress
楔入构造活动是秦岭造山带的成山模型。
So Wedging was the mechanism for mountain building in the Qinling orogen.
天水渭北地区地处祁连与北秦岭造山带结合部位。
Weibei area is located in the joint of the Qilian and North Qinling orogenic belts.
陕西商南县松树沟橄榄岩体是秦岭造山带中具重要意义和争议较大的岩体。
The Songsugou peridotite in Shangnan, Shaanxi Province is an important but petrogenetically debated ultramafic massif in the Qinling orogenic belt.
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