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本文论述了新疆干旱地区因地质构造运动的影响，由古生代石炭纪到新生代第三纪、第四纪的盐类沉积层被隆起接近地表或裸露地面，成为现代土壤盐分的主要来源。
This article discusses the influence of the tectonic movement in the arid region of Xinjiang. From the Paleozoic Carboniferous to the Cenozoic Tertiary, Quaternary sedimentary salt layers are uplifted close to the surface or bare ground and become the main source of modern soil salinity.