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Multidimensional isotropic and anis
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Contents 2.3. Deviation from plane
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Contents 8.3. Inversion of 3D model
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List of Figures 2.1. Amplitude of t
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List of Figures 4.17. Visual repres
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List of Figures 8.2. Ambient noise
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List of Figures 10.10.RMS misfit va
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List of Figures A.15.Result of anis
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List of Tables xviii 5.5. Parameter
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List of Acronyms FE finite element
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List of Symbols Below is a list of
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Symbol SI unit Denotation φ · pha
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Abstract The Tajo Basin and Betic C
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Publications Poster presentations x
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Acknowledgements Team, namely Colin
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Introduction 1 The Iberian Peninsul
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ections from enhanced one-dimension
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Part I Theoretical background of ma
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2. Sources for magnetotelluric reco
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2. Sources for magnetotelluric reco
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2. Sources for magnetotelluric reco
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2. Sources for magnetotelluric reco
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2. Sources for magnetotelluric reco
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2. Sources for magnetotelluric reco
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2. Sources for magnetotelluric reco
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2. Sources for magnetotelluric reco
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2. Sources for magnetotelluric reco
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2. Sources for magnetotelluric reco
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2. Sources for magnetotelluric reco
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Mathematical description of electro
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yields 3.2. Deriving magnetotelluri
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3.2. Deriving magnetotelluric param
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3.3. Magnetotelluric induction area
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Depth d s d 1 d 2 d n-2 d n-1 t 1 t
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3.4. Boundary conditions materials
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3.5. The influence of electric perm
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3.5. The influence of electric perm
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3.5. The influence of electric perm
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Distortion of magnetotelluric data
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4.1. Types of distortion Fig. 4.1.:
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4.1. Types of distortion Fig. 4.3.:
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J s 0 s 0 4.1. Types of distortion
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4.1. Types of distortion Fig. 4.7.:
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Scale Type Terminology Example Atom
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4.1. Types of distortion the use of
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4.2. Dimensionality Fig. 4.12.: The
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1D 2D local 3D/1D 3D/2D regional 4.
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4.3. General mathematical represent
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4.4. Removal of distortion effects
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Parameter Geoelectrical application
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4.4. Removal of distortion effects
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4.4.5. Caldwell-Bibby-Brown phase t
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4.4. Removal of distortion effects
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Method Applicability Swift angle 2D
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5. Earth’s properties observable
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5. Earth’s properties observable
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5. Earth’s properties observable
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5. Earth’s properties observable
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5. Earth’s properties observable
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5. Earth’s properties observable
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5. Earth’s properties observable
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5. Earth’s properties observable
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5. Earth’s properties observable
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5. Earth’s properties observable
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5. Earth’s properties observable
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5. Earth’s properties observable
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6. Using magnetotellurics to gain i
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6. Using magnetotellurics to gain i
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6. Using magnetotellurics to gain i
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6. Using magnetotellurics to gain i
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6. Using magnetotellurics to gain i
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6. Using magnetotellurics to gain i
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6. Using magnetotellurics to gain i
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6. Using magnetotellurics to gain i
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6. Using magnetotellurics to gain i
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6. Using magnetotellurics to gain i
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6. Using magnetotellurics to gain i
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6. Using magnetotellurics to gain i
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Part II Geology of the study area I
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7. Geology of the Iberian Peninsula
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7. Geology of the Iberian Peninsula
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7. Geology of the Iberian Peninsula
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7. Geology of the Iberian Peninsula
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7. Geology of the Iberian Peninsula
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7. Geology of the Iberian Peninsula
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7. Geology of the Iberian Peninsula
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7. Geology of the Iberian Peninsula
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7. Geology of the Iberian Peninsula
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7. Geology of the Iberian Peninsula
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7. Geology of the Iberian Peninsula
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7. Geology of the Iberian Peninsula
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7. Geology of the Iberian Peninsula
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7. Geology of the Iberian Peninsula
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7. Geology of the Iberian Peninsula
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7. Geology of the Iberian Peninsula
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7. Geology of the Iberian Peninsula
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Recovering a synthetic 3D subsurfac
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direction direction Depth: 12 - 30
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8.2. Generating synthetic 3D model
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Distance from the centre of the mes
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3D N45W 3D-crust TE Rho TE Phi Peri
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8.3. Inversion of 3D model data sch
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Model variation RMS misfit Optimal
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Profile: 3D-crust (TM-only) Depth (
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Parameter Value 8.3. Inversion of 3
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Depth (km) 10 -2 10 -1 10 0 10 1 10
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Depth (km) 10 -2 10 -1 10 0 10 1 10
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Step 1: Isotropic 2D inversion Step
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8.3. Inversion of 3D model data par
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8.4. Summary and conclusions bution
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Regularisation order Smoothing para
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S N 1% 0 Depth (km) 3% Depth (km) 1
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9.1. Profile location Data collecti
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Location (degrees) Recording period
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Geological region Stations Geologic
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9.4. Segregation of data acquired w
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Phase (degrees) 135 90 45 0 Z xy -4
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0 km 10 km 30 km 100 km 300 km Dept
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0 km 10 km 30 km 100 km 300 km Dept
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0 km 10 km 30 km 100 km 300 km Dept
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0 km 10 km 30 km 100 km 300 km Dept
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Pseudo-sections crustal strike dire
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9.8. Analysis of vertical magnetic
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9.8. Analysis of vertical magnetic
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10. Data inversion WinGLink softwar
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a (horizontal smoothing) 10. Data i
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10. Data inversion Short period ran
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10. Data inversion TM+TE Depth (km)
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10. Data inversion (a) Constrained
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10. Data inversion the model into u
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10. Data inversion Depth (km) S N 0
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Depth (km) 10. Data inversion S N 0
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10. Data inversion Group velocity m
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10. Data inversion ductivity of thi
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10. Data inversion Shtrikman upper
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10. Data inversion TM+TE Depth (km)
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10. Data inversion TM+TE Depth (km)
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10. Data inversion in the lithosphe
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10. Data inversion isotropic 2D lay
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10. Data inversion Depth (km) Depth
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10. Data inversion Depth (km) Depth
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10. Data inversion Depth (km) Depth
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10. Data inversion tigation is usua
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Depth (km) Depth (km) 10. Data inve
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Modelled Observed Modelled Observed
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Depth (km) 10. Data inversion 0 30
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10. Data inversion Depth off LAB (k
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10. Data inversion Depth (km) S 0 5
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10. Data inversion 10.3. Summary an
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10. Data inversion owing to availab
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11 Summary and conclusions The key
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11.2. PICASSO Phase I investigation
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11.2. PICASSO Phase I investigation
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11.2. PICASSO Phase I investigation
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A. Appendix Eocene 54 Ma 42 Ma 36 M
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A. Appendix A.2. Auxiliary informat
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A. Appendix 292 Fig. A.3.: Issues i
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A. Appendix A.2.4. Computation time
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296 3D-mantle profile Inversion res
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298 07-centre profile The profile 0
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300 3D-crust profile The profile 3D
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302 J-centre profile The J-centre p
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- Page 346 and 347: A. Appendix Anisotropy Resistivity
- 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
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- 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
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- Page 395 and 396: Bibliography Serson, P. H. (1973),
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