关键词: 华县, 岳阳, 地震烈度衰减, 逆时针旋扭, 无震感地带

Abstract: In 1556, seismic shocks occurred in Huaxian, Shanxi Province, and in Yueyang, Hunan Province. Whether the seismic shocks belong to one earthquake? For this purpose, we studied the attenuation of seismic intensity, the similarity of the isoseismal forms of several strong earthquakes in and near Huaxian area, and the W-E-trending Qinling tectonic belt acting as a barrier for the seismic wave propagation. The results show that the boundary of seismic intensity IV of the great Huaxian earthquake lies in Xiangyang-Guangshan zone, near the 23℃ N. That is to say, there is an aseismic belt between Huaxian and Yueyang, and south of the aseismic belt there is another high-seismic intensity area up to VII. For that the epicenter must be near Yueyang, From where the seismic intensity attenuated outward and a closed boundary of intensity contour was formed. It indicates that the earthquake occurring in Yueyang is simultaneous but independent from the Huaxian earthquake in 1556. After then the high seismic frequency in Yueyang area lasted about 20 years. It means a period during which the regional stress was adjusted after the earthquake, whereas the anticlockwise rotational deformation in the upper part of Cisi Pagoda in Yueyang might result from the strong earthquake.

Key words: Huaxian, Yueyang, Seismic intensity attenuation, Anti-clockwise rotational deformation, Aseismic belt