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Simualtion results of T wave proapgation from regions near the Sofu seamount and the Sumisu Caldera - MaRDI portal

Simualtion results of T wave proapgation from regions near the Sofu seamount and the Sumisu Caldera

From MaRDI portal
Dataset:6706768



DOI10.5281/zenodo.11947887Zenodo11947887MaRDI QIDQ6706768

Dataset published at Zenodo repository.

Author name not available (Why is that?)

Publication date: 17 June 2024

Copyright license: No records found.



The simulation results used in the submitted manuscript Simulation results of high-frequency T-wave propagation from regions near the Sofug seamount and the Sumisu Caldera sac.tar: envelopes of simulation results green_sofugan: source grids and index information for simulation results in the region near the Sofugan Volcano green_sumisu: source grids and index information for simulation results in the region around the Sumisu Caldera The characteristics of simulated envelopes were listed in 231009GF_M.KMB06_???.dat (near the Sofu seamount) and 180506GF_M.KMB06_???.dat (Sumisu Caldera). longitude, latitude, depth, epicental distance, theoretical P traveltime, peak arrival time of body wave, theoretical T traveltime, peak arrival time of T wave, half-value starting, half-value ending, mximuma body wave amplitude, maximum T wave amplitude, envelope file name Details are described in "Takemura,S.,Kubota,T., Sandanbata,O.(2024).Successive tsunamigenic events near Sofu Seamount inferred from high-frequency teleseismicPand regionalTwaves.Journal of Geophysical Research: Solid Earth,129, e2024JB029746.https://doi.org/10.1029/2024JB029746"






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