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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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- Page 325 and 326: Miocene (Aquitanian - Langhian) 21
- Page 327 and 328: A.2.2. Oblique strike intricacy A.2
- Page 329 and 330: A.2.3. Jones Catechism A.2. Auxilia
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- Page 333 and 334: 297 04-centre profile The profile 0
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- Page 337 and 338: 301 G-centre profile The profile G-
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- Page 341 and 342: Anisotropy Resistivity Misfit r xx
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- Page 345 and 346: Anisotropy Resistivity Misfit RMS r
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- Page 359: A.4. Auxiliary figures of the Tajo
- Page 362 and 363: Bibliography Amaru, M. L. (2007), G
- Page 364 and 365: Bibliography Bahr, K. (1988), Inter
- Page 366 and 367: Bibliography Brace, W., A. Orange,
- Page 368 and 369: Bibliography Colmenero, J., L. Fern
- Page 370 and 371: Bibliography Duba, A. G., H. C. Hea
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Bibliography Franke, A., R.-U. Bör
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Bibliography Goes, S., W. Spakman,
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Bibliography Heise, W., and J. Pous
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Bibliography Ji, S., S. Rondenay, M
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Bibliography Karato, S., Z. Wang, B
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Bibliography Ledo, J., C. Ayala, J.
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Bibliography Martí, A., P. Queralt
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Bibliography Morgan, J. W., and E.
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Bibliography Osipova, I. L. (1983),
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Bibliography Platt, J., and R. Viss
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Bibliography Rebollal, B. M., and A
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Bibliography Schmeling, H. (1986),
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Bibliography Siripunvaraporn, W. (2
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Bibliography Teixell, A., G. Bertot
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Bibliography van Keken, P. E. (2003
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Bibliography Weidelt, P. (1975), El
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Bibliography Zielhuis, A., and G. N