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Chapter 13 Modelling Seismic Wave Propagation for Geophysical Imaging

Whakaatu ērā atu putanga (1)

The Earth is an heterogeneous complex media from the mineral composition scale (10−6m) to the global scale ( 106m). The reconstruction of its structure is a quite challenging problem because sampling methodologies are mainly indirect as potential methods (Günther et al., 2006; Rücker et al., 2006)...

Whakaahuatanga katoa

I tiakina i:
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Kaituhi matua: Tago, J. (auth)
Ētahi atu kaituhi: Cruz-Atienza, V. (auth), Chaljub, E. (auth), Brossier, R. (auth), Coutant, O. (auth), Garambois, S. (auth), Prieux, V. (auth), Operto, S. (auth), Mercerat, D. (auth), Virieux, J. (auth), Ribodetti, A. (auth)
Hōputu: Tāhiko Wāhanga pukapuka
Reo:Ingarihi
I whakaputaina: InTechOpen 2012
Ngā marau:
Science: general issues
seismic wave
geophysical imaging
Boundary value problem
Finite element method
Free surface
Frequency domain
Seismology
Time domain
Velocity
Urunga tuihono:DOAB: download the publication
DOAB: description of the publication
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DOAB: download the publication
DOAB: description of the publication

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