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Titlebook: Earthquake Hazard and Seismic Risk Reduction; Serguei Balassanian,Armando Cisternas,Mikael Melku Book 2000 Springer Science+Business Media

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樓主: Corticosteroids
21#
發(fā)表于 2025-3-25 05:49:42 | 只看該作者
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發(fā)表于 2025-3-25 09:53:00 | 只看該作者
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發(fā)表于 2025-3-25 14:32:04 | 只看該作者
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發(fā)表于 2025-3-25 18:01:33 | 只看該作者
https://doi.org/10.1007/978-3-031-44738-9ublic of Armenia, the Georgian Academy of Sciences and the Swiss Seismological Service and granted by the Swiss Disaster Relief. The network, which became operational in 1990 and since then gradually extended, consists today of 12 digital free-field stations as well as 6 digital strongmotion instrum
25#
發(fā)表于 2025-3-25 20:28:26 | 只看該作者
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發(fā)表于 2025-3-26 02:24:10 | 只看該作者
https://doi.org/10.1007/978-981-16-6827-2sing both historical chronicles and results of revision of monuments for parameterization of ancient earthquakes, namely, for reconstruction of date, location of epicenter, definition of hypocenter depth, macroseismic effect and intensity. This approach has been extensively used by Georgian seismolo
27#
發(fā)表于 2025-3-26 07:14:05 | 只看該作者
Some Stylized Facts About Central Banks,ose correlation with the features of geomorphological conditions. On the other hand, this relation is not simple. There can be vividly observed a multifactor phenomenon of correlation. The above-mentioned circumstance imposes certain (definite) restrictions on the direct use of the data of macroseis
28#
發(fā)表于 2025-3-26 12:00:04 | 只看該作者
29#
發(fā)表于 2025-3-26 16:30:11 | 只看該作者
The Kathmandu Valley Earthquake Risk Management Project (KVERMP): Project Motivation and Descriptionproject, selected project activities, and the progress of the project as of August 1998 are described below. The project activities discussed are the simplified earthquake scenario and action plan, the school seismic safety program, and public awareness and institution building activities.
30#
發(fā)表于 2025-3-26 18:50:22 | 只看該作者
Brainstem and Midbrain Lesions,quakes with M≈. are described there. But the study of seismic history still is incomplete because these publications did not used regional instrumental catalogues. Our study is devoted to that very problem: study of seismic regime of the Spitak earthquake source vicinity based on the regional scale instrumental catalogue.
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