This paper holds that the measurement data,both from Panzhang fluid levelling and from Zhangdaokou short levelling,are the mid-short term anomalies of Tangshan earthquake.Its anomalous deformation value is lar-get than that in the epicentral area.It is of“stress adjustment element”.
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郑熙铭.唐山7.8级地震前天津地区的一些地形变特征[J].地震工程学报,1985,7(1):44-47. Zheng Ximing. SOME CHARACTERISTICS OF DEFORMATION IN TIANJIN REGION BEFORE TANGSHAN EARTHQUAKE(M=7.8)[J]. China Earthquake Engineering Journal,1985,7(1):44-47.