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DSR represents deep strong reflector discovered by Park et al. (2002b).
The late Jurassic Chiltan Limestone can be recognized easily as a strong reflector on these lines at around 2.5sec TWT.
Although basement-cutting faults offset the TIC, the TIC is not always a continuous, strong reflector in between basement-cutting faults within the study area, as seen on the eastern section of line D02 (Figure 5A).
A returning echo produced by a strong reflector located in the side lobes will be displayed as if it originated from the main beam [ 18- 27, 27].
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(2) Strong reflectors occur at depths of approximately 3 km.
Strong reflectors were found at a depth of approximately 3 km.
We found clear strong reflectors beneath the southern coast of the Boso Peninsula.
Strong reflectors can be observed at a depth of about 3 km towards the north of the lava dome.
CFAR processing is useful for detecting strong reflectors in the background clutter and has widely been used in man-made objects detection from SAR images.
These strong reflectors were interpreted as the upper surface of the subducting PHS plate from their locations and the estimated velocities beneath the reflectors.
We imaged many strong reflectors with a heterogeneous distribution in the deep section (Fig. 7(a)), and observed several distinctive features.
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