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漳河漳县段沿西秦岭北缘断层发育,其南岸保存了良好的四级阶地,Ⅰ级阶地为堆积阶地,局部为基座阶地,Ⅱ、Ⅲ级阶地为基座阶地,Ⅳ级阶地为侵蚀阶地。漳河阶地上覆堆积物特点反映了其形成主要受构造抬升控制,气候变化影响较小。漳河阶地的抬升速率指示了西秦岭北缘地区在晚更新世中晚期经历了短暂的缓和隆升后,全新世以来具有加速隆升的趋势。阶地发育频率可能受到了气候变化的影响使其与隆升速率不具有正相关性。
Zhanghe Zhangzhang fault along the northern margin of the West Qinling development, the south bank of the preservation of a good four terraces, Ⅰ terrace terraces, partial basement terrace, Ⅱ, Ⅲ terraces as the base terrace, Ⅳ terrace Eroded terraces. The characteristics of the overlying sediments in the Zhanghe River terrace reflect that its formation is mainly controlled by tectonic uplift and has less impact on climate change. The rate of uplift of the Zhanghe terraces indicates that the northern margin of the West Qinling Mountains experienced a transient uplift in the late Late Pleistocene and accelerated uplift since the Holocene. The terrestrial development frequency may be affected by climate change so as not to have a positive correlation with the uplift rate.