P. Schmoldt, PhD - MTNet - DIAS

8. Recovering a synthetic 3D subsurface model using lower-dimensional inversion schemes
Fig. 8.19.: Results of anisotropic 2D inversion of the synthetic 3D model for a selection of profiles, from left to right: 3D-crust-west with stations synM11 – synC01, 3D-crust-NS with stations
synE02 – synL09, and 3D-crust-east with stations synN10 – synD00, as well as 3D-crust-EW profile with stations synD10 – synM01 (upper most plot); see Figures 8.4 and 8.5 for location of
stations and profiles. Results are plotted in respect to the station locations; see black lines in the inset on the top-right of the figure. The solid black line in the main plot indicates the projected
location of the 3D-crust-EW profile result (model shown on the top of this Figure), and red inverted triangles on the 3D-crust-EW profile denote location of intersection by the other profiles.
Dashed lines indicate resistivity interfaces of the synthetic 3D model at crust (red) and mantle (blue) depth (cf. Fig. 8.3). For orientation, side panels are shown, which indicate regions of the
synthetic 3D model by colour, following the colouring of the synthetic model. More detailed inversion results for the four profiles are given in Section A.3.2 (Figs. A.15 - A.18). 198
synN10
synM11
1.60
synM05
synL09
synL04
1.60
ynK08
2.35
synK03
1.98
synJ07
syn J02
synH10
synI06
3.10
synI01
2.35
synG09
synF08
1.60
synH05
synG04
3.85
2.73
synE07
2.05
synF03
synD06
synE02
Log10(Wm) 4.60
synD00
3.10
Log 10(Wm)
2.50
2.95
synC01
Log10(Wm) 3.40
250
300
1.60
Depth (km)
150
200
Log 10(Wm)
1.98
2.35
0
50
100
2.73
3.10
W E
synD10
synE09
synF08
synG07
synH06
synI05
synJ04
synK03
synL02
synM01
N
N