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Fig. 2 Post-stack time migrated section of KR101.
The near-surface faults and the larger fault that was continued to larger times were also imaged better in the migrated section of the FO-CDS stacked result.
Pre-stack depth migrated section of the line JFD1 (Figure 3) clearly shows the characteristic structure of the Japan Trench subduction zone at the location of the JFAST drill site C0019.
The color scale shows percentage deviation from the mean (44) Fig. 5 Post-stack time migrated section of KR103 in the top figure (a) and its SAP in the bottom one (b).
The color scale shows percentage deviation from the mean (42) in the whole profile Fig. 4 Post-stack time migrated section of KR102 in the top figure (a) and its SAP in the bottom one (b).
The seafloor reflection is contaminated by artifacts, caused by sideswipes from adjacent slopes, whereas the subducting plate stratigraphy is clearly resolved at a relatively constant two-way travel time of 10,000 to 10,500 ms. Figure 6 Post- stack time migrated section of the line JFS12.
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Open image in new window Fig. 6 Pre and post-migrated section of dipping event.
Compared with the time-migrated sections of multi-channel reflection surveys (Nakamura et al., 2011; 2013), the shallow earthquakes landward of the trench axis mainly occurred in the oceanic crust (Figure 3).
In this way, each point on the migrated section is treated independently from the other points.
Therefore, more events with more details are imaged in the final migrated section.
The migrated sections showed that the FO-CDS method can clearly define the body of mud volcanoes that was not imaged well by other methods.
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