WebJan 13, 2015 · The slip model obtained from geodetic data represents the large scale features of asperities within the megathrust, which is appropriate for simulation of long‐period waves and tsunami modeling. For the simulation of a broadband strong ground motion, we add small scale heterogeneities to the source slip to be able to simulate high … Webment model was made on the basis of forward modeling (Oada 1985, 1992)eferring to the c-seismic data of Subarya et˚.(2006)Chlieh et˚.(2007)h the plate convergence rate of 14/ar (Bet˚. 2005) is use. Earthquakes occurring with a magnitude w ≥4.6and M depth range of H≤50km around the island of Sumatra dating fr19632016e selecte.We found that
Re-examination of Slip Distribution of the 2004 Sumatra–Andaman ...
WebThe coseismic model shows that the Sunda subduction megathrust ruptured over a distance of about 1500 km and a width of less than 150 km, releasing a total moment of 6.7-7.0 × 1022 N m, equivalent to a magnitude Mw ∼9.15. ... Coseismic slip and afterslip of the great M w 9.15 Sumatra-Andaman earthquake of 2004. / Chlieh, Mohamed; Avouac ... WebOct 8, 2024 · General diagram of an oceanic subduction zone. Sumatra and the Andaman Islands are part of an island arc. this figure is taken from the online edition of This Dynamic Earth The December 26, 2004 M=9.1 Sumatra-Andaman earthquake occurred along a tectonic subduction zone in which the India Plate, an oceanic plate, is being subducted … high high high high high high high
Coseismic slip and afterslip of the great Mw 9.15 Sumatra …
WebMay 27, 2024 · Download Firmware: Firmware File: Download [Hi8SE-GMSO.O1.V10.16.RC-V05.8735W] Download SP Flash tool – Make sure that you have … WebFinite-Fault Model Maps – Map representation of the finite-fault model, in GEOJSON and PNG formats. Data and Model Fits ... and the 2004 M w 9.1 Sumatra earthquake had a … WebDanny Hilman Natawidjaja,1,2 Kerry Sieh,1 Mohamed Chlieh,1 John Galetzka,1 Bambang W. Suwargadi, 3 Hai Cheng, 4 R. Lawrence Edwards, 4 Jean-Philippe Avouac, 1 and Steven N. Ward 5 high high high high high high