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Assessment of the Efficiency of Armenian Seismological Networks

机译:评估亚美尼亚地震网络效率

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For successful prediction of strong earthquakes, seismic risk zoning, and earthquake-resistant construction, it is necessary above all to have a sufficiently clear understanding of the hypocentral distribution of earthquakes in the area in question. In order to determine the position of earthquake foci with high accuracy, it is necessary to have an observation system capable of this. The modern seismological network in the Republic of Armenia (RA) essentially consists of two independent networks that barely interact with each other. Moreover, each network uses its own data processing methods (for determining hypocenters and travel-time curves). One network belongs to the National Seismic Protection Service under the Ministry of Emergencies of the Republic of Armenia (NSPS RA) and consists of 16 stations; the other is subordinate to the Institute of Geology of RA National Academy of Sciences (IG NAS RA) and hosts 14 seismic stations. Both networks are set up unevenly in the territory of Armenia, and each has its own disadvantages. The IG NAS RA network is sparser (with only 14 stations), and its stations are located only in northwestern Armenia. Therefore, it cannot accurately localize the hypocenters of earthquakes throughout the republic. The NSPS RA network consists of 16 stations. They are also located unevenly across Armenia, but at the same time, they encompass the southeastern part of the country. Calculations have been performed and maps compiled of the distribution of minimum energy classes and maximum errors in determining hypocentral coordinates of earthquakes recorded both separately by the IGN NAS RA and NSPS RA networks and by the integrated seismic network. It is shown that when the networks are combined, localization of earthquake hypocenters improves somewhat, but the territory between northwestern and southeastern Armenia remains virtually uncovered. This is because, at present, the stations of both existing networks, on the one hand, duplicate each other in some cases, while on the other, they are located unevenly across the territory. To obtain more accurate and reliable information, it is better to have a single network with be uniformly placed throughout the republic.
机译:为了成功地预测强烈地震,地震风险分区和抗震结构,最重要的是对有问题地区的地震斜视分布有足够清楚的了解。为了以高精度确定地震灶的位置,有必要具有能够实现的观察系统。亚美尼亚共和国(RA)的现代地震网络基本上由两个独立网络组成,几乎没有互相互动。此外,每个网络都使用其自身的数据处理方法(用于确定斜视和行进时间曲线)。一个网络属于亚美尼亚共和国紧急情况部的国家地震保护服务(NSPRA),由16个站组成;另一个是隶属于RA国家科学院地质研究所(IG NAS RA)和举办14个地震站。两个网络在亚美尼亚境内不均匀地建立,每个网络都有自己的缺点。 IG NAS RA网络是稀疏(只有14个站),其站仅位于亚美尼亚西北部。因此,它无法准确地定位整个共和国地震的震中。 NSP RA网络由16个站组成。它们也在亚美尼亚不均匀地定位,但同时,它们包括该国的东南部。已经执行计算并编制的映射最小能量类和最大误差在确定由IGN NAS RA和NSP RA网络和集成地震网络单独记录的地震的斜视坐标时。结果表明,当网络组合时,地震效率的定位有所改善,但西北和亚美尼亚之间的领土几乎没有发现。这是因为,目前,现有网络的站点一方面在某些情况下彼此重复,而另一方面,它们位于该领域的不均匀。为了获得更准确和可靠的信息,最好在整个共和国统一地放置一个网络。

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