In this paper,based on the data of virtual investigation,the author has discussed the characteristics of deformation band and earthquake frac-ture of Gulang earthquke in 1927 and analysed the geotectonical back-ground of this earthquake.The author helieves that the occurrence of Gulang earthquake in1927 Was the result that the fracture band of Tazhuang-Huangcheng andthat of Wuwei-Tianzhu were in activity at the sametime.And based no the analysis of their rupturing way,the mechanics model of fragmentation massif movement has been made.
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贾云鸿.1927年古浪大震地质构造背景及其成因的初步探讨[J].地震工程学报,1982,4(3):78-82. Jia Yun-hong. PRELIMINARY DISCUSSION OF GEOTECTONICAL BACKGROUND AND GENESIS OF GULANG STRONG EARTHQUAKE IN 1927[J]. China Earthquake Engineering Journal,1982,4(3):78-82.