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pro vyhledávání: '"Thomas van Stiphout"'
We describe a model-based approach to forecast seismic risk during an earthquake sequence, emphasizing building damage and human injuries. This approach, which could also be used to forecast financial losses, incorporates several models of varying co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d98cbcce866caf452dfad8e9a6e63d85
https://doi.org/10.1016/b978-0-12-394848-9.00007-9
https://doi.org/10.1016/b978-0-12-394848-9.00007-9
Autor:
Surya P. Acharya, John G. Anderson, Masataka Ando, Kuvvet Atakan, John Bevington, Glenn P. Biasi, Roger Bilham, James N. Brune, Victor Chebrov, James E. Daniell, Ranjan Dhungel, Amod M. Dixit, M. Eineder, C. Geiß, Matthew C. Gerstenberger, Marcus Herrmann, Mitsuyuki Hoshiba, Charles Huyck, Mizuho Ishida, Vladimir G. Kossobokov, Mustapha Meghraoui, Gero W. Michel, Anastasia Nekrasova, Giuliano Panza, Imtiyaz A. Parvez, Antonella Peresan, M. Pittore, Philippe Rosset, K. Saito, Tom Schacher, Danijel Schorlemmer, Surya N. Shrestha, E. So, Gennady Sobolev, Mark W. Stirling, H. Taubenböck, Stavros V. Tolis, Thomas van Stiphout, Enrica Verrucci, M. Wieland, Stefan Wiemer, Zhongliang Wu, Max Wyss, J. Douglas Zechar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f728d544c69178ab25a029d95aab9bce
https://doi.org/10.1016/b978-0-12-394848-9.01002-6
https://doi.org/10.1016/b978-0-12-394848-9.01002-6
Publikováno v:
Bulletin of the Seismological Society of America
Identifying changes in the rate of background earthquakes is a common method to detect transients in seismic-activity rates, and these transients can often be linked to changes in physical properties of the crust or to the recording homogeneity of se
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1a127adfb931526524c7b375df235515
https://gfzpublic.gfz-potsdam.de/pubman/item/item_243520
https://gfzpublic.gfz-potsdam.de/pubman/item/item_243520
Publikováno v:
Geophysical Research Letters. 37
[1] The disastrous earthquake in L'Aquila Italy (Mw 6.3, 6 April 2009) again highlights the issue of potentially reducing seismic risk by releasing warnings or initiating mitigation actions. Earthquakes cluster strongly in space and time, leading to