P. Schmoldt, PhD - MTNet - DIAS
P. Schmoldt, PhD - MTNet - DIAS P. Schmoldt, PhD - MTNet - DIAS
A. Appendix Anisotropy Resistivity Misfit r xx Depth (km) 100 150 200 250 300 0 rAA 50 Depth (km) Depth (km) RMS -1 0 1 2 3 4 TM -1 0 1 2 3 4 Log 10(periods) -2 S N 0 50 100 150 200 250 300 0 ryy 50 TE Log 10(periods) -2 100 150 200 250 300 pic020 pic019 0 15 30 45 60 75 90 105 120 135 Distance (km) Apparent resistivity Log10(Wm) Phase degrees pic020 pic019 pic017 pic015 pic013 pic011 pic009 pic007 pic006 pic005 pic004 pic003 pic002 pic001 pic017 pic015 pic013 pic011 pic009 Log 10(Wm) pic007 pic006 pic005 pic004 pic003 pic002 pic001 Total: Log10(rxx)-Log10(ryy) Log10(Wm) Log10(Wm) pic020 pic019 pic017 pic015 pic013 pic011 pic009 pic007 pic006 pic005 pic004 pic003 pic002 pic001 4.30 4.0 3.4 2.8 2.2 1.6 4.0 3.4 2.8 2.2 1.6 degrees Fig. A.11.: Result of anisotropic 2D inversion for the 3D-mantle profile with stations pic001 - pic020 on top of the synthetic 3D model (cf. Figs. 8.3, 8.4, and 8.5 for synthetic 3D model, station location, and profile location) following the second anisotropic inversion approach (cf. 8.3.3). Station data is decomposed according to the strike direction of the mantle (N45E), and laplacian regularisation and an increased smoothing parameter (τ = 6) are used for the inversion. Isotropic inversion of long-period data in the first sequence (hence the similarity of ρxx and ρyy at depth > 30 km) is followed by anisotropic inversion of short-period data in the second sequence. See Section 8.3.3 regarding current limitations of the approach. 304
Anisotropy Resistivity Misfit r xx Depth (km) 100 150 200 250 300 0 rAA 50 Depth (km) Depth (km) RMS -1 0 1 2 3 4 TM -1 0 1 2 3 4 Log 10(periods) -2 0 50 100 150 200 250 300 0 ryy 50 TE Log 10(periods) -2 100 150 200 250 300 pic020 pic019 A.4. Auxiliary figures of the Tajo Basin subsurface investigation pic017 S N 0 17 34 51 68 85 102 119 136 153 Distance (km) Apparent resistivity Log10(Wm) Phase degrees pic020 pic019 pic017 pic015 pic013 pic011 pic009 pic007 pic006 pic005 pic004 pic003 pic002 pic001 pic015 pic013 pic011 pic009 pic007 pic006 pic005 pic004 pic003 pic002 pic001 Log 10(Wm) Log 10(Wm) Log 10(r xx)-Log 10(r yy) Total: 0.53 3.40 2.95 2.50 2.05 1.60 3.20 2.80 2.40 2.00 1.60 Log 10(Wm) degrees pic020 pic019 pic017 pic015 pic013 pic011 pic009 pic007 pic006 pic005 pic004 pic003 pic002 pic001 Fig. A.12.: Result of anisotropic 2D inversion for the 3D-crust profile with stations pic001 - pic020 on top of the synthetic 3D model (cf. Figs. 8.3, 8.4, and 8.5 for synthetic 3D model, station location, and profile location). Station data is decomposed according to the strike direction of the crust (N45W), and inversion is carried out with resistivity gradient regularisation and an increased smoothing parameter (τ = 6), following the first inversion approach: isotropic inversion of short-period data in the first sequence and anisotropic inversion of long-period data in the second sequence. 305
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- Page 296 and 297: 10. Data inversion Depth (km) Depth
- Page 298 and 299: 10. Data inversion tigation is usua
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- Page 302 and 303: Modelled Observed Modelled Observed
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- Page 312 and 313: 10. Data inversion owing to availab
- Page 315 and 316: 11 Summary and conclusions The key
- Page 317 and 318: 11.2. PICASSO Phase I investigation
- Page 319 and 320: 11.2. PICASSO Phase I investigation
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- Page 324 and 325: A. Appendix Eocene 54 Ma 42 Ma 36 M
- Page 326 and 327: A. Appendix A.2. Auxiliary informat
- Page 328 and 329: A. Appendix 292 Fig. A.3.: Issues i
- Page 330 and 331: A. Appendix A.2.4. Computation time
- Page 332 and 333: 296 3D-mantle profile Inversion res
- Page 334 and 335: 298 07-centre profile The profile 0
- Page 336 and 337: 300 3D-crust profile The profile 3D
- Page 338 and 339: 302 J-centre profile The J-centre p
- Page 342 and 343: A. Appendix Anisotropy Resistivity
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- Page 348 and 349: A. Appendix A.4. Auxiliary figures
- Page 350 and 351: A. Appendix 314 ρ TE(Ω−m) φ T
- Page 352 and 353: A. Appendix 316 ρ TE(Ω−m) φ T
- Page 354 and 355: A. Appendix 318 ρ TE(Ω−m) φ T
- Page 356 and 357: A. Appendix 320 pic003 (off-diagona
- Page 358 and 359: A. Appendix 322 pic013 (off-diagona
- Page 361 and 362: Bibliography Abalos, B., J. Carrera
- Page 363 and 364: Bibliography Artemieva, I. M. (2006
- Page 365 and 366: Bibliography Berdichevsky, M., V. D
- Page 367 and 368: Bibliography Cebriá, J.-M., and J.
- Page 369 and 370: Bibliography de Vicente, G., J. Gin
- Page 371 and 372: Bibliography Egbert, G. D., and J.
- Page 373 and 374: Bibliography Ganapathy, R., and E.
- Page 375 and 376: Bibliography Haak, V., and R. Hutto
- Page 377 and 378: Bibliography Hutton, R. (1972), Som
- Page 379 and 380: Bibliography Jones, A. G., and R. W
- Page 381 and 382: Bibliography Kurtz, R. D., J. A. Cr
- Page 383 and 384: Bibliography Lviv Centre of Institu
- Page 385 and 386: Bibliography Merrill, R. T., and M.
- Page 387 and 388: Bibliography Newman, G., and G. Hoh
- Page 389 and 390: Bibliography Pádua, M. B., A. L. P
A. Appendix<br />
Anisotropy Resistivity<br />
Misfit<br />
r xx<br />
Depth (km)<br />
100<br />
150<br />
200<br />
250<br />
300<br />
0<br />
rAA 50<br />
Depth (km)<br />
Depth (km)<br />
RMS<br />
-1<br />
0<br />
1<br />
2<br />
3<br />
4<br />
TM<br />
-1<br />
0<br />
1<br />
2<br />
3<br />
4<br />
Log 10(periods) -2<br />
S N<br />
0<br />
50<br />
100<br />
150<br />
200<br />
250<br />
300<br />
0<br />
ryy 50<br />
TE<br />
Log 10(periods) -2<br />
100<br />
150<br />
200<br />
250<br />
300<br />
pic020<br />
pic019<br />
0 15 30 45 60 75 90 105 120 135<br />
Distance (km)<br />
Apparent resistivity Log10(Wm) Phase<br />
degrees<br />
pic020<br />
pic019<br />
pic017<br />
pic015<br />
pic013<br />
pic011<br />
pic009<br />
pic007<br />
pic006<br />
pic005<br />
pic004<br />
pic003<br />
pic002<br />
pic001<br />
pic017<br />
pic015<br />
pic013<br />
pic011<br />
pic009<br />
Log 10(Wm)<br />
pic007<br />
pic006<br />
pic005<br />
pic004<br />
pic003<br />
pic002<br />
pic001<br />
Total:<br />
Log10(rxx)-Log10(ryy) Log10(Wm) Log10(Wm) pic020<br />
pic019<br />
pic017<br />
pic015<br />
pic013<br />
pic011<br />
pic009<br />
pic007<br />
pic006<br />
pic005<br />
pic004<br />
pic003<br />
pic002<br />
pic001<br />
4.30<br />
4.0<br />
3.4<br />
2.8<br />
2.2<br />
1.6<br />
4.0<br />
3.4<br />
2.8<br />
2.2<br />
1.6<br />
degrees<br />
Fig. A.11.: Result of anisotropic 2D inversion for the 3D-mantle profile with stations pic001 - pic020 on top of the synthetic 3D<br />
model (cf. Figs. 8.3, 8.4, and 8.5 for synthetic 3D model, station location, and profile location) following the second anisotropic<br />
inversion approach (cf. 8.3.3). Station data is decomposed according to the strike direction of the mantle (N45E), and laplacian<br />
regularisation and an increased smoothing parameter (τ = 6) are used for the inversion. Isotropic inversion of long-period data in the<br />
first sequence (hence the similarity of ρxx and ρyy at depth > 30 km) is followed by anisotropic inversion of short-period data in the<br />
second sequence. See Section 8.3.3 regarding current limitations of the approach.<br />
304
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