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Integral Evolution Pattern of Intraplate Seismicity in Chinese Mainland and Its Periphery
作者姓名:Liu WenyiThe Second Crustal Deformation Monitoring Center  SSB  Xi'an  China
作者单位:Liu WenyiThe Second Crustal Deformation Monitoring Center,SSB,Xi'an 710054,China
摘    要:Taking the active fault network as the structural frame, the Chinese mainland and its periphery can be regarded as a system of "fault movement and seismogeny." By using the self-coupling method, preliminary study shows that the seismogenic system is a time-ordered dissipation system. The time order in the state far from equilibrium is established and maintained through mass and energy exchanges between the system and the surroundings. The evolution of the seismogenic system follows some properties of unbalanced phase change, namely, critical retard, bifurcation, entropy reduction, etc.

关 键 词:Autocorrclation,  Correlation  analysis,  Seismic  activity,  Evolution  pattern.

Integral Evolution Pattern of Intraplate Seismicity in Chinese Mainland and Its Periphery
Liu WenyiThe Second Crustal Deformation Monitoring Center,SSB,Xi'an ,China.Integral Evolution Pattern of Intraplate Seismicity in Chinese Mainland and Its Periphery[J].Earthquake Research in China,1997(1).
Authors:Liu WenyiThe Second Crustal Deformation Monitoring Center  SSB  Xi'an  China
Institution:Liu WenyiThe Second Crustal Deformation Monitoring Center,SSB,Xi'an 710054,China
Abstract:
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