5月12日,四川省汶川县发生里氏8.0地震,山崩地裂、灾难袭来,席卷了四川十几个县市,波及全国十几个省市,灾区人民的生命和财产遭受了极大的损失,面对突如其来的特大灾害,社会各界紧急行动,向灾区人民伸出援手。由中国书画艺术委员会、听...5月12日,四川省汶川县发生里氏8.0地震,山崩地裂、灾难袭来,席卷了四川十几个县市,波及全国十几个省市,灾区人民的生命和财产遭受了极大的损失,面对突如其来的特大灾害,社会各界紧急行动,向灾区人民伸出援手。由中国书画艺术委员会、听雨楼文化艺术公司、北京中国书画协会、丽池会所管理集团、《Best Life ·香格里拉》展开更多
The ground motion attenuation models for PGA,PGV and response spectrum at rock sites and soils sites are derived separately from the digital strong motion records of moderate earthquakes in the Sichuan-Yunnan region a...The ground motion attenuation models for PGA,PGV and response spectrum at rock sites and soils sites are derived separately from the digital strong motion records of moderate earthquakes in the Sichuan-Yunnan region after 2007. By comparison with Yu Yanxiangs attenuation model for rock sites in western China,reliability of the model is verified for moderate earthquake. According to the distribution of strong motion data against magnitude and epicentral distance,the applicability and reliability of the results in this paper are discussed.展开更多
This paper presents the damage in the meizoseismal region of the M_S8.0 Wenchuan earthquake,Sichuan,China,and the seismic intensities determined according to "the Chinese Seismic Intensity Scale",and discuss...This paper presents the damage in the meizoseismal region of the M_S8.0 Wenchuan earthquake,Sichuan,China,and the seismic intensities determined according to "the Chinese Seismic Intensity Scale",and discusses briefly the types of earthquake-generating faults and some features of seismic damage.展开更多
Based on GPS data from 1991- 2004 and the least-squares collocation method,we analyze the crustal deformation in the Chinese mainland. The results show that the first-order crustal deformation is unchanged in differen...Based on GPS data from 1991- 2004 and the least-squares collocation method,we analyze the crustal deformation in the Chinese mainland. The results show that the first-order crustal deformation is unchanged in different periods in the Chinese mainland,which reflects the background of regional tectonic activity. The strain rate is much higher in Western China,especially in the Qinghai-Tibetan Plateau and Sichuan-Yunnan area. The variations in different periods are related with seismicity of strong earthquakes during the same time. The GPS data after 2004 shows the post-seismic deformation of the 2001 Kunlun Mountains M S8. 1 earthquake.展开更多
文摘5月12日,四川省汶川县发生里氏8.0地震,山崩地裂、灾难袭来,席卷了四川十几个县市,波及全国十几个省市,灾区人民的生命和财产遭受了极大的损失,面对突如其来的特大灾害,社会各界紧急行动,向灾区人民伸出援手。由中国书画艺术委员会、听雨楼文化艺术公司、北京中国书画协会、丽池会所管理集团、《Best Life ·香格里拉》
基金sponsored jointly by the special fund for basic research and operating expenses of Institute of Crustal Dynamics,CEA(ZDJ2013-04)"National Nature Science Foundation of China(51278469)
文摘The ground motion attenuation models for PGA,PGV and response spectrum at rock sites and soils sites are derived separately from the digital strong motion records of moderate earthquakes in the Sichuan-Yunnan region after 2007. By comparison with Yu Yanxiangs attenuation model for rock sites in western China,reliability of the model is verified for moderate earthquake. According to the distribution of strong motion data against magnitude and epicentral distance,the applicability and reliability of the results in this paper are discussed.
文摘This paper presents the damage in the meizoseismal region of the M_S8.0 Wenchuan earthquake,Sichuan,China,and the seismic intensities determined according to "the Chinese Seismic Intensity Scale",and discusses briefly the types of earthquake-generating faults and some features of seismic damage.
基金funded by the Science and Technology Support Program(2012BAK19B01)Natural Science Foundation of China(41104057,41104058)the special project of basic scientific research of Institute of Earthquake Science,China Earthquake Administration(2012IES0405,2012IES0406)
文摘Based on GPS data from 1991- 2004 and the least-squares collocation method,we analyze the crustal deformation in the Chinese mainland. The results show that the first-order crustal deformation is unchanged in different periods in the Chinese mainland,which reflects the background of regional tectonic activity. The strain rate is much higher in Western China,especially in the Qinghai-Tibetan Plateau and Sichuan-Yunnan area. The variations in different periods are related with seismicity of strong earthquakes during the same time. The GPS data after 2004 shows the post-seismic deformation of the 2001 Kunlun Mountains M S8. 1 earthquake.
