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根据大量的野外现场考察资料，对1125年兰州7．0级地震形变破裂带的特征以及庄浪河断裂带晚第四纪以来的活动性进行了初步研究，探讨了该次地震的宏观震中位置及其构造背景。并在古地震破裂形迹分析的基础上，运用年代学资料，对庄浪河断裂带全新世以来的古地震事件等问题作了讨论。
Based on a large number of field investigation data, the characteristics of the deformed crustal zone of Lanzhou MS 7.0 earthquake in 1125 and the activity since the late Quaternary of the Zhuanglanghe Fault Zone have been studied. The macro epicenter location And its tectonic background. On the basis of the analysis of the ancient earthquake rupture, the authors used the chronological data to discuss the paleoearthquakes and other issues since the Holocene in the Zhuanglanghe fault zone.