Crustal heterogeneity as inferred from seismic coda wave decomposition by small-aperture array observation
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Cited by (13)
Chapter 11 Imaging Inhomogeneous Structures in the Earth by Coda Envelope Inversion and Seismic Array Observation
2008, Advances in GeophysicsCitation Excerpt :We introduce some of the recent studies with remarkable results in this section. Wave types (P or S waves) and propagating directions of wave trains in the coda part of seismograms have been studied (e.g., Scherbaum et al., 1997; Kuwahara et al., 1997). Especially, detailed studies based on the array observations with three‐component seismometers were performed by Wagner (1998) and Taira (2004).
Aso94: Aso seismic observation with broadband instruments
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2013, Geophysical Journal InternationalSeismic wave propagation and scattering in the heterogeneous earth: Second edition
2012, Seismic Wave Propagation and Scattering in the Heterogeneous Earth: Second Edition
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