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P. Schmoldt, PhD - MTNet - DIAS

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Contents<br />

8.3. Inversion of 3D model data . . . . . . . . . . . . . . . . . . . . . . . . . 178<br />

8.3.1. Isotropic 2D inversion of 3D model data . . . . . . . . . . . . . . 179<br />

8.3.2. Anisotropic 1D inversion of 3D model data . . . . . . . . . . . . 184<br />

8.3.3. Anisotropic 2D inversion of 3D model data . . . . . . . . . . . . 189<br />

8.4. Summary and conclusions . . . . . . . . . . . . . . . . . . . . . . . . . 194<br />

IV. Magnetotelluric investigation of the southern Iberian subsurface<br />

- PICASSO Phase I 200<br />

9. Data collection and processing 201<br />

9.1. Profile location . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 201<br />

9.2. Analysis of collected data . . . . . . . . . . . . . . . . . . . . . . . . . . 205<br />

9.3. Correction of faulty records in electric channels of long-period instruments 205<br />

9.4. Segregation of data acquired with the long-period systems according to<br />

phase values . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 207<br />

9.5. Merging broadband and long-period data . . . . . . . . . . . . . . . . . . 208<br />

9.6. Compensating for distortion of the impedance tensor . . . . . . . . . . . 210<br />

9.6.1. Geoelectric strike estimation . . . . . . . . . . . . . . . . . . . . 210<br />

9.6.2. Decomposition of the impedance tensor . . . . . . . . . . . . . . 218<br />

9.7. Analysis of TE and TM mode response data . . . . . . . . . . . . . . . . 218<br />

9.8. Analysis of vertical magnetic transfer function data . . . . . . . . . . . . 221<br />

10. Data inversion 225<br />

10.1. Inversion for crustal structures . . . . . . . . . . . . . . . . . . . . . . . 226<br />

10.1.1. Determining smoothing parameters for inversion . . . . . . . . . 226<br />

10.1.2. Starting model construction . . . . . . . . . . . . . . . . . . . . 228<br />

10.1.3. Investigating characteristics of TE and TM mode response data . 231<br />

10.1.4. Evaluating proposed layered crustal model . . . . . . . . . . . . 233<br />

10.1.5. Final model of the Tajo Basin crust . . . . . . . . . . . . . . . . 235<br />

10.2. Inversion for mantle structures . . . . . . . . . . . . . . . . . . . . . . . 246<br />

10.2.1. Isotropic 2D inversion . . . . . . . . . . . . . . . . . . . . . . . 247<br />

10.2.2. Anisotropic 1D inversion . . . . . . . . . . . . . . . . . . . . . . 255<br />

10.2.3. Anisotropic 2D inversion . . . . . . . . . . . . . . . . . . . . . . 256<br />

10.2.4. Isotropic 3D inversion . . . . . . . . . . . . . . . . . . . . . . . 261<br />

10.3. Summary and conclusions . . . . . . . . . . . . . . . . . . . . . . . . . 274<br />

iv

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