P. Schmoldt, PhD - MTNet - DIAS
P. Schmoldt, PhD - MTNet - DIAS P. Schmoldt, PhD - MTNet - DIAS
A. Appendix A.4. Auxiliary figures of the Tajo Basin subsurface investigation A.4.1. Responses for crustal inversion model This Section contains responses for the PICASSO Phase I stations and the isotropic 2D subsurface model for the Tajo Basin crust shown in Figure 10.6. Responses are displayed in terms of apparent resistivity and impedance phase values for periods ≤ 10 3 s that are related to the crustal depth range (cf. Sec. 10.1). TE mode data are shown on the lefthand side, whereas TM mode data are shown on the right-hand side of each figure. Also shown are the RMS misfit values for both modes at the bottom of each figure as well as the average RMS misfit at the top of each figure. 312 ρ TE(Ω−m) φ TE(degrees) RMS TE 10 2 10 1 0 −30 −60 1.44 −90 1.08 0.72 0.36 10 −2 10 −1 10 0 10 1 10 2 10 3 Site: pic001 RMS: 0.835134257769307 ρ TM(Ω−m) φ TM(degrees) RMS TM 10 1 0 −30 −60 1.76 −90 1.32 0.88 0.44 TE TM Orig Model 10 −2 10 −1 10 0 10 1 10 2 10 3 Fig. A.19.: Comparison of observed data for station pic001 and the related model response for the model shown in Figure 10.6.
ρ TE(Ω−m) φ TE(degrees) RMS TE 10 2 0 −30 −60 −90 1.8 1.2 0.6 A.4. Auxiliary figures of the Tajo Basin subsurface investigation 0.0 10−2 10−1 100 101 102 103 Site: pic002 RMS: 1.10800695361517 ρ TM(Ω−m) φ TM(degrees) RMS TM 10 2 10 1 0 −30 −60 −90 2.58 1.72 0.86 0.00 TE TM Orig Model 10 −2 10 −1 10 0 10 1 10 2 Fig. A.20.: Comparison of observed data for station pic002 and the related model response for the model shown in Figure 10.6. ρ TE(Ω−m) φ TE(degrees) RMS TE 10 2 0 −30 −60 −90 0.84 0.56 0.28 0.00 10−2 10−1 100 101 102 103 Site: pic003 RMS: 0.493181745536071 ρ TM(Ω−m) φ TM(degrees) RMS TM 10 2 10 1 0 −30 −60 −90 0.75 0.50 0.25 TE TM Orig Model 0.00 10−2 10−1 100 101 102 103 Fig. A.21.: Comparison of observed data for station pic003 and the related model response for the model shown in Figure 10.6. 313
- Page 298 and 299: 10. Data inversion tigation is usua
- Page 300 and 301: Depth (km) Depth (km) 10. Data inve
- Page 302 and 303: Modelled Observed Modelled Observed
- Page 304 and 305: Depth (km) 10. Data inversion 0 30
- Page 306 and 307: 10. Data inversion Depth off LAB (k
- Page 308 and 309: 10. Data inversion Depth (km) S 0 5
- Page 310 and 311: 10. Data inversion 10.3. Summary an
- 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
- Page 321: 11.2. PICASSO Phase I investigation
- 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 340 and 341: A. Appendix Anisotropy Resistivity
- Page 342 and 343: A. Appendix Anisotropy Resistivity
- Page 344 and 345: A. Appendix Anisotropy Resistivity
- Page 346 and 347: A. Appendix Anisotropy Resistivity
- 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
- Page 391 and 392: Bibliography Prácser, E., and L. S
- Page 393 and 394: Bibliography Ritter, J. R. R., M. J
- Page 395 and 396: Bibliography Serson, P. H. (1973),
- Page 397 and 398: Bibliography Spitzer, K. (2006), Ma
ρ TE(Ω−m)<br />
φ TE(degrees)<br />
RMS TE<br />
10 2<br />
0<br />
−30<br />
−60<br />
−90<br />
1.8<br />
1.2<br />
0.6<br />
A.4. Auxiliary figures of the Tajo Basin subsurface investigation<br />
0.0<br />
10−2 10−1 100 101 102 103 Site: pic002 RMS: 1.10800695361517<br />
ρ TM(Ω−m)<br />
φ TM(degrees)<br />
RMS TM<br />
10 2<br />
10 1<br />
0<br />
−30<br />
−60<br />
−90<br />
2.58<br />
1.72<br />
0.86<br />
0.00<br />
TE TM Orig Model<br />
10 −2 10 −1 10 0 10 1 10 2<br />
Fig. A.20.: Comparison of observed data for station pic002 and the related model response for the model shown in Figure 10.6.<br />
ρ TE(Ω−m)<br />
φ TE(degrees)<br />
RMS TE<br />
10 2<br />
0<br />
−30<br />
−60<br />
−90<br />
0.84<br />
0.56<br />
0.28<br />
0.00<br />
10−2 10−1 100 101 102 103 Site: pic003 RMS: 0.493181745536071<br />
ρ TM(Ω−m)<br />
φ TM(degrees)<br />
RMS TM<br />
10 2<br />
10 1<br />
0<br />
−30<br />
−60<br />
−90<br />
0.75<br />
0.50<br />
0.25<br />
TE TM Orig Model<br />
0.00<br />
10−2 10−1 100 101 102 103 Fig. A.21.: Comparison of observed data for station pic003 and the related model response for the model shown in Figure 10.6.<br />
313