P. Schmoldt, PhD - MTNet - DIAS
P. Schmoldt, PhD - MTNet - DIAS P. Schmoldt, PhD - MTNet - DIAS
A. Appendix Eocene 54 Ma 42 Ma 36 Ma Oligocene 30 Ma 27 Ma 24 Ma Fig. A.1.: Geological evolution of the Iberian Peninsula in terms of past and present-day stress fields; figures and related description from Andeweg [2002] - this Figure is continued on the next page (Fig. A.2). Main tectonic events relevant for the Iberian Peninsula for the period displayed by this figure: uplift of the Hesperic Massif (basement in western and Central Iberia) due to ENE-WSW extension with perpendicular compression, before that only the western part of the present Iberian Peninsula was emerged (54 Ma); the southern margin of the Iberian Peninsula deepens southward, thrust loading of the margin by Internal Betic units is likely (42 Ma); Uplift of the Spanish Central System (SCS) (36 Ma); Internal Betics crustal segments are stacking, resulting in an over-thickening and subsequent extensional deformation of the Internal Betics (36 Ma); inversion of the Iberian Basin starts (30 Ma); first uplift of the Sierra Altomira (24 Ma). 288
Miocene (Aquitanian - Langhian) 21 Ma 18 Ma 15 Ma A.1. Geological evolution of the Iberian Peninsula Miocene (Serravallian - Messinian) 12 Ma 9 Ma 6 Ma Pliocene + Quaternary 3 Ma 0 Ma Fig. A.2.: Geological evolution of the Iberian Peninsula in terms of past and present-day stress fields - continued from Figure A.1. Main tectonic events relevant for the Iberian Peninsula for the period displayed by this figures: onset of collision between the Betics and the southern Iberian margin, resulting in compression and folding in the Eastern Prebetics (21 Ma); elevation of the SCS (15 Ma); collision of the Internal Betics with the southern margin of Iberia, resulting in major inversions throughout the entire Iberian Peninsula (12 Ma); SCS thrusts over Duero and Tajo Basins (12 Ma); thrusting of the Subbetics over the eastern Prebetics and submergence of the western External Prebetics (12 Ma); Uplift of the whole Betics, resulting in withdrawal of the sea and disconnection from marine Mediterranean or Atlantic waters (6 Ma). 289
- Page 274 and 275: 10. Data inversion Depth (km) S N 0
- Page 276 and 277: Depth (km) 10. Data inversion S N 0
- Page 278 and 279: 10. Data inversion Group velocity m
- Page 280 and 281: 10. Data inversion ductivity of thi
- Page 282 and 283: 10. Data inversion Shtrikman upper
- Page 284 and 285: 10. Data inversion TM+TE Depth (km)
- Page 286 and 287: 10. Data inversion TM+TE Depth (km)
- Page 288 and 289: 10. Data inversion in the lithosphe
- Page 290 and 291: 10. Data inversion isotropic 2D lay
- Page 292 and 293: 10. Data inversion Depth (km) Depth
- Page 294 and 295: 10. Data inversion Depth (km) Depth
- Page 296 and 297: 10. Data inversion Depth (km) Depth
- 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 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 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.
Miocene<br />
(Aquitanian<br />
- Langhian)<br />
21 Ma 18 Ma 15 Ma<br />
A.1. Geological evolution of the Iberian Peninsula<br />
Miocene<br />
(Serravallian<br />
- Messinian)<br />
12 Ma 9 Ma 6 Ma<br />
Pliocene<br />
+<br />
Quaternary<br />
3 Ma 0 Ma<br />
Fig. A.2.: Geological evolution of the Iberian Peninsula in terms of past and present-day stress fields - continued from Figure A.1.<br />
Main tectonic events relevant for the Iberian Peninsula for the period displayed by this figures: onset of collision between the Betics<br />
and the southern Iberian margin, resulting in compression and folding in the Eastern Prebetics (21 Ma); elevation of the SCS (15 Ma);<br />
collision of the Internal Betics with the southern margin of Iberia, resulting in major inversions throughout the entire Iberian Peninsula<br />
(12 Ma); SCS thrusts over Duero and Tajo Basins (12 Ma); thrusting of the Subbetics over the eastern Prebetics and submergence of<br />
the western External Prebetics (12 Ma); Uplift of the whole Betics, resulting in withdrawal of the sea and disconnection from marine<br />
Mediterranean or Atlantic waters (6 Ma).<br />
289
Change language