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A 3-D Shear Wave Velocity Model for Myanmar Region
ArticleAbstract: Myanmar is located at the eastern margin of the ongoing Indo-Eurasian collision system, has experienPalabras claves:Bayesian inversion, crustal structure, MYANMAR, seismic velocity model, waveform simulationAutores:Anna E. Foster, Banerjee P., Bodin T., Huang B.S., Hubbard J.A., Maung Maung P., Moe Oo K., Rafael V. Almeida, Wang X., Wang Y., Wei S.Fuentes:scopusA slip gap of the 2016 M<inf>w</inf> 6.6 Muji, Xinjiang, China, Earthquake Inferred from Sentinel-1 TOPS Interferometry
ArticleAbstract: We use Sentinel-1A/1B Terrain Observation with Progressive Scans (TOPS) data to map coseismic and poPalabras claves:Autores:Feng W., Liu P., Rafael V. Almeida, Samsonov S.V., Tian Y., Zhang Y.Fuentes:googlescopusEnhanced stress and changes to regional seismicity due to the 2015 M<inf>w</inf> 7.8 Gorkha, Nepal, earthquake on the neighbouring segments of the Main Himalayan Thrust
ArticleAbstract: In this study we evaluate stress evolution and change in seismic hazard after the 2015 Gorkha earthqPalabras claves:Brownian Passage Time model, Coulomb stress change, Nepal earthquake, Rate-and-state aftershock forecast model, Renewal seismic hazard modelAutores:Chan C., Rafael V. Almeida, Wang Y., Yadav R.Fuentes:googlescopusSlip rate deficit and earthquake potential on shallow megathrusts
ArticleAbstract: Most destructive tsunamis are caused by seismic slip on the shallow part of offshore megathrusts. ThPalabras claves:Autores:Bradley K.E., Burgmann R., Hill E.M., Hubbard J.A., Lindsey E.O., Mallick R., Moore J.D.P., Rafael V. AlmeidaFuentes:googlescopusSource characteristics of the 2015 M<inf>W</inf> 7.8 Gorkha (Nepal) earthquake and its M<inf>W</inf> 7.2 aftershock from space geodesy
ArticleAbstract: On April 25, 2015, a destructive MW 7.8 earthquake struck the capital of Nepal, Kathmandu, killing mPalabras claves:ALOS2, Elastic layering, Gorkha earthquake, InSAR modeling, Sentinel-1 A, The Main Frontal Thrust fault (MFT)Autores:Barbot S., Chen J., Dai K., Feng W., Li P., Li Z., Lindsey E.O., Rafael V. Almeida, Samsonov S.V., Xu X.Fuentes:googlescopusStructural segmentation controlled the 2015 M<inf>W</inf> 7.8 Gorkha earthquake rupture in Nepal
ArticleAbstract: The ongoing collision of India with Asia is partly accommodated by slip on the Main Himalayan ThrustPalabras claves:Autores:Anna E. Foster, Bürgi P., Hubbard J.A., Rafael V. Almeida, Sapkota S.N., Tapponnier P.Fuentes:scopusStructure of the Tokai segment from the integrated high-resolution seismic imaging - a case study from the eastern Nankai Trough
Conference ObjectAbstract: Subduction zones around the world remain one of the most important targets of geophysical investigatPalabras claves:Autores:Brossier R., Górszczyk A., Métivier L., Rafael V. AlmeidaFuentes:googlescopusThe effects of core-reflected waves on finite fault inversions with teleseismic body wave data
ArticleAbstract: Teleseismic body waves are essential for imaging rupture processes of large earthquakes. EarthquakePalabras claves:Body waves, Computational seismology, Earthquake source observations, Waveform inversionAutores:Ni S., Qian Y., Rafael V. Almeida, Wei S., Zhang H.Fuentes:googlescopusSeismic imaging of the Main Frontal Thrust in Nepal reveals a shallow décollement and blind thrusting
ArticleAbstract: Because great earthquakes in the Himalaya have an average recurrence interval exceeding 500 yr, mostPalabras claves:Himalayan earthquakes, Main Frontal Thrust, Paleoseismology, reflection seismic, tectonic geomorphologyAutores:Anna E. Foster, Hubbard J.A., Liberty L., Rafael V. Almeida, Sapkota S.N.Fuentes:scopusRe-evaluating seismic hazard along the southern Longmen Shan, China: Insights from the 1970 Dayi and 2013 Lushan earthquakes
ArticleAbstract: Competing hypotheses have been proposed to explain the seismic hazard (i.e. whether earthquakes withPalabras claves:Gutenberg-Richter law, Longmen Shan, Seismic hazard, Seismic moment, Seismogenic structure, Wenchuan earthquakeAutores:Hubbard J.A., Li Z., Liu-Zeng J., Rafael V. Almeida, Sun C., Yi G.Fuentes:googlescopus