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Tectonic forces from the relative movements between plates are transmitted into the continental crust, and then they create the earthquake generating stress field there. The space-time distribution of the seismic activity including the small earthquakes in a region reflects the variation of the stress field in the region. According to this idea, the characteristics of the stress fields in the various regions of East Asia have been analyzed in detail in this paper based on a lot of solutions of focal mechanisms and data of seismic activity during the last 500 years. The results indicate that the tectonic forces from the subduction of the Pacific Ocean plate underneath the Eurasian plate control the stress field in the region from North China to the northern part of the North-South Seismic Belt. The variation of the regional stress field shown by the variation of seismic activity in some regions of Japan has also been discussed based on characteristics of variation of the seimicity of small earthquakes. Synchronous variations of seismicity in the past 100 years or so in West China and in the boundary region between the Indo-Australian and Eurasian plates implicate that there is the transmission of tectonic forces into West China through the collision between the Indo-Australian and Eurasian plates. The active seismic activity in the boundary region between the Indo-Australian and the Eurasian plates and in West China is continuing consistently. The Chinese version of this paper appeared in the Chinese edition ofActa Seismologica Sinica,13, 287–294, 1991.  相似文献   
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Introduction Zhangjiakou-Bohai seismic zone is a major active seismic zone that passes through the north-ern part of North China. Zhangjiakou-Beijing area, the northwest part of North China, is located at the intersection position of Yanshan, Taihangshan uplift, and Shanxi down-faulted zone, and the geological structures in this area are extremely complicated. Many researchers in the geoscience circle always pay close attention to this region because Yanqing-Huailai region is located in th…  相似文献   
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不是所有的活断层都会发生强震,其中只有极少数在几十年或几百年内,有可能发生强震,这里将它们特称为"强震发生断层"."强震发生断层"不是一个简单的面,而是有一定宽度的板状体.板状体是受了多期破裂而形成的疏松破碎的夹持层,错动时产生围限波,使强震发生断层内烈度陡增.新建的重要建筑物应避开"强震发生断层";不能避开的,则要提高建筑物的抗震能力.台湾集集1999年7.6级地震,石冈大坝地区0.15 g的抗震设防,竟能抗御0.5 g的影响,不少民房坏而不倒,尚可住人值得借鉴.  相似文献   
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IntroductionMaximumentropyspectralmethod(MEM)(Burg,1972)hadbeenamethodusuallyusedinstudyingtheseismicityanditsmainpurposeistofindthedominantspectrainthelong-termseismicityprocessesinthepastyears(Zhu,1985).Inthispaper,themethodisappliedtostudywhethertherearesomespecialspectraofseismicityinsomespecificstagesinearthquake-generatingprocesses.Sowestudyseparatelythenormalandabnormalstageofearthquakeactivity,whoseactiveprocessisregardedasstablestochasticprocess,inordertofindtheirspectracharactersan…  相似文献   
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本文对由十余条深部地震测深部面观测结果综合归纳出来的一个华北地区岩石圈上部12层三维非均匀模型,进行了应力场计算,并根据计算结果对唐山地震孕育背景及长期前兆异常特征进行了分析讨论。  相似文献   
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