A homogeneous dilated sphere in the hemi-infinite elastic space is ta-ken as the mechanical model of the quickly uplifted mantle.With this model the radius and the dilative intensity of the sphere can be com-puted from the value of the vertical displacement on the earth's surfa-ce.The supplementary stress deduced from the uplifted is determined.The computing result showes that the deduced stress on the fault with high inclined angle is tensile,but the shearing stress is also found in the upliftel region of the earth's crust.The amount of these stresses deduced from the quickly uplifted mantle greatly overcomes the stresses deduced from the gravimetric earth-tide,the diviation of the polar axis and the variation of rotational velocity of earth.Consequently,the quickly uplifted mantle has more trigger action than above-menti-oned factors for the occurance of the shallow tectonic earthquake.Ow-ing to the fact that many large earthquakes occur ed recently in China have been affected in the uplifted region of earth's crust or in its ne-ighborhood and these earthquake faults have high inclined angle,their occurance can be explained by the results described in this paper.
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丁文镜.地幔快速隆起对构造地震的触发作用[J].地震工程学报,1982,4(2):58-66. Ding Wen-jing. THE TRIGGER ACTION OF THE QUICKLY UPLIFTED MANTLE FOR THE SHELLOW TECTONIC EARTHQUAKE[J]. China Earthquake Engineering Journal,1982,4(2):58-66.