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Constraints on the shallow deformation around the Main Frontal Thrust in central Nepal from refraction velocities
ArticleAbstract: The youngest fault system in the Himalayan orogeny is the Main Frontal Thrust (MFT), the frontal ramPalabras claves:Main Frontal Thrust, Nepal Himalaya, P-wave velocity, Sediment thickness, Seismic refraction, Water tableAutores:Anna E. Foster, Hubbard J.A., Lee Y.S., Liberty L., Liu Y., Rafael V. Almeida, Sapkota S.N.Fuentes:scopusFluvial Sedimentary Response to Late Quaternary Climate and Tectonics at the Himalayan Frontal Thrust, Central Nepal
ArticleAbstract: To investigate the subsurface structure surrounding the Main Frontal Thrust (MFT) in central Nepal,Palabras claves:Boreholes, fluvial environment, fold-and-thrust belt, Himalaya, Indian monsoon, Main Frontal ThrustAutores:Haines S.H., Hamahashi M., Hubbard J.A., Mishra S., Owen L.A., Rafael V. Almeida, Sapkota S.N.Fuentes:googlescopusOblique Thrusting and Strain Partitioning in the Longmen Shan Fold-and-Thrust Belt, Eastern Tibetan Plateau
ArticleAbstract: Eastern Tibet is an important example of oblique convergence and associated strain partitioning, asPalabras claves:eastern Tibet, Longmen Shan, Oblique thrusting, Strain partitioning, Wenchuan earthquakeAutores:Hubbard J.A., Jia D., Li T., Li Z., Rafael V. Almeida, Shi X., Sun C., Zhang P., Zheng W.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:googlescopus