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Geología, hidrología, meteorología(5)
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Hypocentre determination offshore of eastern Taiwan using the maximum intersection method
ArticleAbstract: The maximum intersection (MAXI) method, which derives from the master station method (MSM), determinPalabras claves:3-D, Earthquake, Hypocentre, Location, Outliner, TAIWÁNAutores:Chiao L.Y., Kao H., Lallemand S.E., Liu C.S., Yvonne FontFuentes:scopusUpper-plate structure in Ecuador coincident with the subduction of the Carnegie Ridge and the southern extent of large mega-thrust earthquakes
ArticleAbstract: The Ecuadorian convergent margin has experienced many large mega-thrust earthquakes in the past centPalabras claves:Crustal Imaging, crustal structure, Seismic noiseAutores:Agurto-Detzel H., Alexandra P. Alvarado, Beck S.L., Charvis P., Hoskins M.C., Koch C.D., Lynner C., Mario C. Ruiz, Meltzer A., Porritt R.W., Regnier M.M., Rietbrock A., Soto-Cordero L., Stachnik J.C., Yvonne FontFuentes:scopusSeismicity patterns along the ecuadorian subduction zone: New constraints from earthquake location in a 3-D a priori velocity model
ArticleAbstract: To improve earthquake location, we create a 3-D a priori P-wave velocity model (3-DVM) that approximPalabras claves:Computational seismology, Seismic cycle, Seismicity and tectonics, SOUTH AMERICA, Subduction zone processesAutores:Mónica Segovia, Sandro Vaca, Theunissen T., Yvonne FontFuentes:scopusStructure of the Ecuadorian forearc from the joint inversion of receiver functions and ambient noise surface waves
ArticleAbstract: The Ecuadorian forearc is a complex region of accreted terranes with a history of large megathrust ePalabras claves:Crustal Imaging, crustal structure, Joint inversion, Seismicity and tectonics, SOUTH AMERICAAutores:Agurto-Detzel H., Alexandra P. Alvarado, Beck S.L., Charvis P., Delph J., Hoskins M.C., Koch C.D., Lynner C., Mario C. Ruiz, Meltzer A., Regnier M.M., Rietbrock A., Soto-Cordero L., Stachnik J.C., Yvonne FontFuentes:scopusThe largest instrumentally recorded earthquake in Taiwan: Revised location and magnitude, and tectonic significance of the 1920 event
ArticleAbstract: The Ryukyu subduction is known to generate very few earthquakes in its central segment contrarily toPalabras claves:Continental margins: convergent, Dynamics: seismotectonics, Seismicity and tectonics, Subduction zone processesAutores:Lallemand S.E., Liang W.T., Theunissen T., Yvonne FontFuentes:scopus