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A reflector at a depth of around 45 km could roughly explain the travel times and amplitudes of signals at offsets of over 180 km.
The deeper reflector at a depth of 3 4 km corresponds to the top of the upper crust based on its V p model (Fig. 7).
They found a planar distribution of the S wave reflection points (S wave reflector) at a depth of 20 30 km.
The ultimate goal of a durability study is to conceive meaningful accelerated testing procedures that simulate real outdoor degradation in a short time and provide service lifetime estimates for a certain type of reflector at a specific site.
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Simulating a perfect reflector at an altitude equal to the virtual height of reflection, the virtual time delay is assumed as a real time delay.
Kaneda et al. (2010) found deeper reflectors at a depth of 35 to 45 km beneath seamounts with a hot spot origin in the northwestern Pacific Basin.
The PD signal is actually a measure of the density of moving reflectors at a particular level, and thus of the fractional vascular volume [ 9, 10].
Depicted in Fig. 4, a single reflector at 1.3 mm depth produced a single peak in the A-line profile.
To increase the system dynamic range, 30 A-scans of a reflector at the same position were averaged.
Figure 3 demonstrates sample A-scans of the reflector at different imaging depths: (A) ~0.22mm, (B) ~1.43mm, (C) ~2.31mm, (D) ~2.60mm, and (E) ~2.90mm.
When imaging the reflection from a tilt-free, planar reflector at the focus of a high numerical microscope objective, all of the incident rays will be collected by the objective, however, for a sphere the angle of reflection of an incident ray at the sphere's surface depends upon the transverse scan position.
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