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《Earthquake Engineering and Engineering Vibration》 1983-04
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INTENSITY OF EARTHQUAKE SEQUENCES

Wu Kaitong Liang Hongguang (Analysis and Prediction Center, State Seismological Bureau)  
This paper discusses the intensity of the earthquake sequences, which include the foreshock, main shock and aftershock. The rock of the area of hypocenter is broken gradually, while the aftershocks continually happen after the mainshock, so that energy of the seismic wave attenuates largely and intensity of the strong aftershocks with the same magnitude will differ when they are in different time order and spatial positions. However, the intensities of the mainshock and foreshock ssetn to have no such effect because the rock is roughly complete.In this paper, The author also points out the intensity distinction between mainshock and early aftershock.
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