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根据野外断层露头、探槽及热释光年龄样数据， 揭示了大同盆地内黄花梁—山自皂断层为公元５１２ 年强震的发震断层。这对确定该次地震宏观震中及研究大同盆地地震活动性具有重要意义。
Based on the data of outcrops, trenches and thermoluminescence ages in the wild, it reveals the seismogenic fault of the Huanghuliang-Shanzao fault in the Datong Basin as a strong earthquake of 512 AD. This is of great significance for determining the macro epicenter of this earthquake and studying the seismicity of the Datong Basin.