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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

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【作者】 赵洪声黄更生罗葆荣杨子汉张淑蓉范杨赵迎浪王世芹

【Author】 Zhao Hongsheng (Seismological Bureau of Yunnan Province)Huang Gengsheng (Meteorological Bureau of Yunnan Province)Luo Baorong(Yunnan Astronomical Observatory)Yang Zhihan Zhang Shurong Fan Yang Zhao Yinglang Wang Shiqin (Seismological Bureau of Yunnan Province)

【机构】 云南省地震局云南省气象局云南天文台云南省地震局

【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.

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