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The deep-seated structures and the earthquakes in Northeast China

Lu Zacxun (Seismological Bureau of Liaoning Province)  
The result cf the study on the deep-seated structures in Norhcast China by usnig the data of geophysical field shows that the whole region of Northeast China is an uplifted area of the upper mantle with NE trending. The middle part, including the Songliao Basin and ihe Xialiaohe Basin, is thinner in the crust thickness with little variation, being about 33-34km. In the west part, i.e.the Greater Xingan Mountains, the crust thickness increases from 35 to 39km, the top plane of the mantle being a steep slope.In the east part are the Zhangguangcai Ridge and the Liaodong Peninsular whose crust thickness obviously increase to about 36-37km. Many faults, such as Yilan-Yi-tong, Hunhe-Dunhua-Mishan, Mudanjiang, Eutehaqi, Longhua-Ningcheng, and Niuju-Youyangou have cut the bottom of the crust with their own characteristics.Through the study of the seismicity, the deep geophysical field and the deep-seated structures, it indicates that the seismic activities in this area are closely related to some special parts of the geophysical field and the deep-seated structures. The distinguished marks of the deep-seated structure variation zone are put forward on this basis. It has been preliminarily proved in practice that the earthquakes, especially large earthquakes usually occured on the deep-seated variation zones. The Haicheng earthquake cf magnitude 7.3 and the Tangshan earthquake of magnitude 7.8 in recent years just happeded on the varition zones. Meanwhile clear precursor anomalies could be observed on these zones. The variation zones of the deep-seated structures in Northeast China delimited preliminarily in this Paper.
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