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应用遥感图像解释并结合野外调查，从宏观角度研究了黄土源区做地貌特征及分市规律，指出这些微地貌的形成与新构造运动有关，它们是在新构造节理裂隙带的基础上形成的。这些微地貌部位有利于黄土裂隙孔洞水的形成与分布，是塬区找水的有利部位。
Using remote sensing image interpretation combined with the field investigation, this paper studied the geomorphic features and the laws of subdivision from the macroscopic perspective, pointing out that the formation of these micro-topographical features is related to the neotectonic movement. They are formed on the basis of the newly constructed fractured zone . These micro-topographical sites are conducive to the formation and distribution of water in the fractured holes in the loess and are favorable sites for water finding in the highland.