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禄劝地震某些成因的宏观研究
MACROSCOPIC RESEARCH ON THE SEISMOGENESIS OF THE 1985 LUQUAN EARTHQUAKE WITH MAGNITUDE=6.3
【摘要】 <正> 作为地球局部构造活动之一的地震事件,其动力来源是很复杂的。许多大震表明,地震系统可能是个开放系统,即其不仅存在着自激过程,且外层空间还有负熵输入。1985年4月18日,昆明市郊禄劝县6.3级地震的孕育和爆发过程,再次为上述观点提供了佐证。本文从这次强震前内、外动力增强的若干直接或间接表现来具体讨论这一问题。
【Abstract】 The Luquan earthquake (Ms=6.3) occured at 102°51"’E, 25°50’N on April 18, 1985, is a typical continental shallow earthquakes with a focal depth of only 5 km. Except a large background of characteristic changes in solar activity before the shock, the seismicity level of moderate shocks around the Luquan area had also obviously increased. In the short-term and impending stage, frequent intrusion of strong weather systems on the ground surface and the enhancement of celestial-body gravitation concerned might excite the final failure of the earthquake-preparation medium. The authors, therefore, consider that the Luquan earthquake (Ms.=6.3) is caused by the step-by-step enhancement and superposition of both internal and external forces in this area in the recent years prior to the event.
- 【文献出处】 地震 ,Earthquake , 编辑部邮箱 ,1986年02期
- 【被引频次】2
- 【下载频次】18