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This work aims to improve the non-uniform temperature distribution of the cross and depth sections of a heated target that is produced by the approximate and skin effects, which often occur in induction heating using a conventional single-layered coil.
Figure 4 shows representative depth sections of the final model.
Figure 4 Depth sections of the final 3-D model.
Figure 3 Depth sections of receiver functions beneath line A to B in Figure1c.
(b) Depth sections of relocated earthquakes in each box shown in Fig. 2(a).
Figure 4 Depth sections of seismic velocities and receiver functions beneath the linear seismic array (along section Y = 0).
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b Depth section of hypocenters and assumed M 5.7 faults.
b Vertical depth section of the relocated hypocenters perpendicular to the NNW SSE orientation.
The depth section of each receiver function was represented by a bending ray with a ray parameter and back azimuth.
The deep section is shown in Fig. 7. Fig. 7 (a) Depth section of the deep section and (b) interpretation of the section.
At depths greater than 40 km, a depth section of receiver functions shows that the oceanic crust is subducting with a dip angle of approximately 15°.
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