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Crustal velocity structure of southern Guatemala using refracted and Sp converted waves

The crustal velocity structure of southern Guatemala is estimated using the methods ofMinimum Apparent Velocity and Converted Waves, applied to local seismic data. Theresults are tested by relocating a random sample of events and by the generation ofsynthetic seismograms. The velocity model obtained...

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Furkejuvvon:
Bibliográfalaš dieđut
Publikašuvnnas:Geofísica Internacional
Váldodahkkit: Juan Pablo Ligorría, Enrique Molina
Materiálatiipa: Artigo
Giella:Inglês
Almmustuhtton: Universidad Nacional Autónoma de México 1997
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Liŋkkat:https://www.redalyc.org/articulo.oa?id=56836102
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