Seismic gravity waves in a sedimentary layer [Ondes sismiques de gravite dans une couche sedimentaire]
Por:
Lomnitz C.
Publicada:
1 ene 1989
Resumen:
An abrupt transition takes place between the elastic and the hydrodynamic regimes when a nonlinear material such as a sediment is subjected to large-amplitude surface waves. The nonlinear transition occurs when the shear strain approaches a critical value ?c. -English summary
Filiaciones:
Lomnitz C.:
Institut de Geophysique, UNAM, 04510 Mexico City, Mexico, Mexico