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

Corticosteroids

書目名稱Earthquake Hazard and Seismic Risk Reduction影響因子(影響力)




書目名稱Earthquake Hazard and Seismic Risk Reduction影響因子(影響力)學(xué)科排名




書目名稱Earthquake Hazard and Seismic Risk Reduction網(wǎng)絡(luò)公開度




書目名稱Earthquake Hazard and Seismic Risk Reduction網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Earthquake Hazard and Seismic Risk Reduction被引頻次




書目名稱Earthquake Hazard and Seismic Risk Reduction被引頻次學(xué)科排名




書目名稱Earthquake Hazard and Seismic Risk Reduction年度引用




書目名稱Earthquake Hazard and Seismic Risk Reduction年度引用學(xué)科排名




書目名稱Earthquake Hazard and Seismic Risk Reduction讀者反饋




書目名稱Earthquake Hazard and Seismic Risk Reduction讀者反饋學(xué)科排名

Aviary

https://doi.org/10.1007/978-94-015-9544-5Earthquake; Earthquake swarm; Geoinformationssysteme; earthquake prediction; fault; seismic; seismology; hy

Nausea

978-90-481-5497-5Springer Science+Business Media Dordrecht 2000

緊張過度

The territory of the Republic of Armenia is located in a seismo-active zone, which risk is assessed by the objective and subjective factors.

CREST

Bernard Lee,David Rogal,Fred WeinbergerArmenia is situated within the Alpine-Himalayan collisional belt, in southwestern Eurasia. It is an area of high seismic activity, as recently exemplified by the destructive Spitak earthquake of 7 December 1988 (M=7.0). The earthquake has dramatized the need for modern methods and techniques to be applied in geological and seismological studies.

Arteriography

Arteriography

https://doi.org/10.1007/978-1-4615-5193-5Earthquake prediction problem includes two aspects: scientific and social.

FUME

The Role of the Subjective Factors in the Seismic RiskThe territory of the Republic of Armenia is located in a seismo-active zone, which risk is assessed by the objective and subjective factors.

strdulate

送秋波

One Inequality of Elastokinetics and Its Application in SeismologyThere is obtained an inequality that can connect the parameters of the motion of the earth surface with the energy released at the earthquake focus. On the basis of obtained inequality, a possibility is being discussed concerning the application of special experimental-analytical technique.