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The background is the optical reflection image of substrate W-AAO2-Au photographed through a microscope with a × 50 objective.
The background is the optical reflection image of substrate CW300 photographed through a microscope with a × 50 objective.
In the reflection image of the RK02 profile, intrusive bodies penetrate the shallow lithosphere and reach the seafloor to form volcanic mounds (Fig. 6).
In the reflection image of RK02, a distinct deep reflector is imaged at the two-way travel time of ~ 5 s, which is equivalent to ~ 9 km depth below the seafloor (Fig. 6).
Black boxes indicate the locations of the close-up images in Figs. 4, 5, 6, 7 and 8 Fig. 4 Seismic reflection image of the RK02 profile focusing on the Tokara Channel.
On the other hand, despite the short distance from the RK01 profile, the reflection image of the RK02 profile is remarkably different from that of the RK01 profile, which is dominated by a series of eastward dipping normal faults forming the half-graben structures on the rotated blocks (Fig. 8).
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We obtained THz reflection images of brain tissues with and without tumors via THz imaging and classified all tumor regions.
They obtained fine reflection images of the magma chambers, faults, and the structure of the graben formed by crustal accretion at the ridge.
Most of them crosscut each other and thus are interpreted to represent a "flower structure" probably caused by strike-slip movements Fig. 8 a Seismic reflection images of the back-arc basin along the RK02 profile and b its interpretation.
On the western part of the basin, normal faults displacing the sedimentary layers are observed (black arrows) Fig. 6 a Seismic reflection images of the RK02 profile showing magmatic intrusion breaching the seafloor.
The reflection images of the intracellular TiO2 nanoparticles and the fluorescence images of nuclei (or Golgi complexes) were simultaneously obtained by the LSCM in two channels with no filter for the reflecting light and a 585 to 640-nm bandpass filter for the fluorescence.
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