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Earth, Planets and Space
Fig. 10 | Earth, Planets and Space

Fig. 10

From: Visualization of attenuation structure and faults in incoming oceanic crust of the Nankai Trough using seismic attenuation profiling

Fig. 10

Enlarged composite profile of conventional seismic reflection and attenuation profiles without fault interpretation (a) and with fault interpretation (b). Seismic reflectivity is effective for imaging geologic structures and faults in the sediments, whereas seismic attenuation is effective for imaging faults in the igneous oceanic crust. Red inverted triangles denote the locations of high-attenuation stripes

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