A Grezio, A Babeyko, MA Baptista… - Reviews of …, 2017 - Wiley Online Library
Applying probabilistic methods to infrequent but devastating natural events is intrinsically challenging. For tsunami analyses, a suite of geophysical assessments should be in …
We develop new empirical scaling laws for rupture width W, rupture length L, rupture area A, and average slip D, based on a large database of rupture models. The database …
EH Field, RJ Arrowsmith, GP Biasi… - Bulletin of the …, 2014 - pubs.geoscienceworld.org
Abstract The 2014 Working Group on California Earthquake Probabilities (WGCEP14) present the time‐independent component of the Uniform California Earthquake Rupture …
Tsunami warning centres face the challenging task of rapidly forecasting tsunami threat immediately after an earthquake, when there is high uncertainty due to data deficiency. Here …
L Blaser, F Krüger, M Ohrnberger… - Bulletin of the …, 2010 - pubs.geoscienceworld.org
Earthquake rupture length and width estimates are in demand in many seismological applications. Earthquake magnitude estimates are often available, whereas the geometrical …
On 11 March 2011, the devastating M9. 0 Tohoku Earthquake occurred on the interface of the subducting Pacific plate, and was followed by a huge tsunami that killed about 20,000 …
S Murotani, K Satake, Y Fujii - Geophysical Research Letters, 2013 - Wiley Online Library
Scaling relations for seismic moment M0, rupture area S, average slip D, and asperity size Sa were obtained for large, great, and giant (Mw= 6.7–9.2) subduction‐zone earthquakes …
TI Allen, GP Hayes - Bulletin of the Seismological …, 2017 - pubs.geoscienceworld.org
Alternative fault‐rupture‐scaling relationships are developed for M w 7.1–9.5 subduction interface earthquakes using a new database of consistently derived finite‐fault rupture …
BE Shaw - Bulletin of the Seismological Society of …, 2023 - pubs.geoscienceworld.org
Scaling relations play an important role in fault‐based seismic hazard estimates. Scaling relations impact estimates of the sizes and rate for a given fault area. Here, we examine …