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81.
By conducting a historical review of this large seismic event in the Mediterranean, it has been possible to identify both the epicentral area and the area in which its effects were principally felt. Ever since the nineteenth century, the seismological tradition has offered a variety of partial interpretations of the earthquake, depending on whether the main sources used were Arabic, Greek or Latin texts. Our systematic research has involved the analysis not only of Arab, Byzantine and Italian chronicle sources, but also and in particular of a large number of never previously used official and public authority documents, preserved in Venice in the State Archive, in the Marciana National Library and in the Library of the Museo Civico Correr. As a result, it has been possible to establish not only chronological parameters for the earthquake (they were previously uncertain) but also its overall effects (epicentral area in Crete, Imax XI MCS). Sources containing information in 41 affected localities and areas were identified. The earthquake also gave rise to a large tsunami, which scholars have seen as having certain interesting elements in common with that of 21 July 365, whose epicentre was also in Crete. As regards methodology, this research made it clear that knowledge of large historical earthquakes in the Mediterranean is dependent upon developing specialised research and going beyond the territorial limits of current national catalogues. 相似文献
82.
Bi Fuzhi Yuan Youshen Institute of Crustal Dynamics State Seismological Bureau Beijing 《《地质学报》英文版》1997,71(4):395-406
This paper expounds the quantitative tectonic indicators and some qualitative indicators of large earthquakes in the coast areas of Fujian, Guangdong, Taiwan and Hainan. The main quantitative indicators include uplift amplitude of the Moho, Quaternary and Late Holocene coasts. The paper also gives a brief account of the research method on quantitative indicators of surface uplifted zones. Taiwan is a famous neotectonic zone and an area of large earthquakes in the world. There is only one large-earthquake area in each of Fujian, Guangdong and Hainan Provinces. Along the coast large earthquake areas there are certainly many remains of crustal activity. Among these remains, coast activity, taking the sea level as the accurate marker horizon, can determine not only the amplitude of coastal elevation and subsidence in a certain period, but also the cycle and rate of positive or negative movements. 相似文献
83.
IntroductionYunnanProvinceislocatedinthesouthofNorth-SouthseismiczoneinChina.ItisoneofthehighseismicactiveregionsinChinesemainland.Morethanonehundredstrongearthquakeswithmagnitude6ormoreoccurredinthisregioninhistory.AsanimportantsoutheasternmarginofTibetanPlateau,YunnanregionisahotspotinstudyonthedynamicsofTibetanPlateau.Theactionsofcompressivestressinnorth-southorientationandgravitationalpotentialcausedlateralextrusionofmaterialintheplateauwiththeupliftingofTibetanPlateau.Severalblocksa… 相似文献
84.
2003年6月17日和7月10日,先后在四川省西昌市和西昌-昭觉间发生2次ML4 8级强有感地震.对于这2次地震,我们曾作了较好的中期和短期预测.但是对于6月17日发生的第一次ML4 8级地震,未能做出临震预测;对于第二次地震,则在7月1日向上级填报的周会商表中作了明确的临震预测,7月10日,在西昌-昭觉间发生了ML4.8级地震.根据西昌地震遥测台网各子台的P波初动求解震源机制,结合地震所处的地质构造以及现场烈度考察圈定出的结果分析,认为这二次地震是由安宁河断裂带、则木河断裂、凉山断裂所围成的凉山小菱形块体活动的结果. 相似文献
85.
86.
云南地区2001年4月10日至6月8日相继发生了4月10日MS5.2、4月12日MS5.9和6月8日MS5.3的施甸地震. 本文利用云南遥测数字地震台网的保山地震台记录的地震波形资料,使用SAM分析方法(即剪切波分裂系统分析方法),采用地震应力预测的分析手段,对这个强震系列进行剪切波分裂参数变化特征的研究. 初步结果表明,随着地震活动的增强,剪切波分裂时间延迟值t基本呈现增加的特征,但在强震即将发生之前的短时间内,发生t减小的现象,符合我们早先研究发现的震前应力释放现象. 研究认为,在地震活动强烈的构造地区和有强震发生危险的经济发达地区或重要城市,开展强烈地震的应力预测应用实践,可以减轻地震的危害程度. 相似文献
87.
88.
地震台站工作人员 ,在进行观测资料分析、地震预报研究过程中 ,往往会遇到的几个问题 :1、手段单一 ,对于前兆现象无法全面表述。 2、如何识别异常与地震之间的关系。 3、如何兼顾点和面的关系。 相似文献
89.
90.
R.M.W. Musson 《Bulletin of Earthquake Engineering》2004,2(1):101-112
Three sites in the UK are taken, representative of low, medium and high hazard levels (by UK standards). For each site, the
hazard value at 10−4 annual probability is computed using a generic seismic source model, and a variety of ground motion parameters: peak ground
acceleration (PGA), spectral acceleration at 10 Hz and 1 Hz, and intensity. Disaggregation is used to determine the nature
of the earthquakes most likely to generate these hazard values. It is found (as might be expected) that the populations are
quite different according to which ground motion parameter is used. When PGA is used, the result is a rather flat magnitude
distribution with a tendency to low magnitude events (\le 4.5 ML) which are probably not really hazardous. Hazard-consistent scenario earthquakes computed using intensity are found
to be in the range 5.8–5.9 ML, which is more in accord with the type of earthquake that one expects to be a worst-case event
in the UK.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献