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quan qiu ms 7 3 4 ji di zhen de ding xiang qian yi
Author(s): Ma Zongjin; Li Xianzhi(Institute of Geology, SSB,Beijing 100029)(Center for Analysis and Prediction,SSB,Beijing 100029)
Pages: 127-
136
Year: 1994
Issue:
2
Journal: Seismology and Geology
Keyword: :Global seismic zones; Orientational migration; Geodynamic interpretation;
Abstract: Based on the analysis of the orientational migration of 184 earthquakes of Ms≥73/4 orgreater along 6 seismic zones which are of a global scale,we found the phenomenom of global ori-entational migration of earthquakes。Generally the migrations take place from the western to theeastern,with their velocities ranging from 700km/a to 140km/a.The global orientational migra-tion of major earthquakes can be interpreted by various geedynamic processes such as the P waveshaped oscillation propagation of the movement of the upper mantle material from the western tothe eastern caused by intermittent extensional break along the Alantic ridge.It can also be inter-preted by eastward propagation of strain wave caused by the sequent SW-NE compression on theEurasia seismic zone from the Africa,Arabia,and India plates;and the NW and NE orientatedoblique compression of the oceanic plate on the both sides of the Pacific ridge.
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