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P. Schmoldt, PhD - MTNet - DIAS

P. Schmoldt, PhD - MTNet - DIAS

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1. Introduction<br />

synthetic model study encourages application of the novel approach to the real PICASSO<br />

Phase I dataset.<br />

Investigation of the Iberian Peninsula subsurface within the framework of the PICASSO<br />

Phase I project is discussed in Part IV: Magnetotelluric investigation of the southern<br />

Iberian subsurface – PICASSO Phase I. Therein, acquisition of the PICASSO Phase I<br />

data is specified (Chapter 9), followed by a description of inversion procedures used to<br />

determine the Tajo Basin crust and mantle structures, and a discussion of the inversion<br />

results (Chapter 10). Processing of the dataset includes, among others, investigation of<br />

geoelectric strike directions for the different regions along the profile as well as the change<br />

of geoelectric strike direction with depth, which leads to the development of the novel<br />

anisotropic inversion approach. Anisotropic 1D and 2D inversion that use the novel approach,<br />

as well as isotropic 2D and 3D inversion is used to derive models of the complex<br />

Iberian Subsurface. Results of 1D, 2D, and 3D approaches are compared with each other,<br />

and results of previous geophysical studies in the region are used in the interpretation of<br />

model features.<br />

Part V: Summary, Appendix, and Bibliography comprises a summary of results for<br />

the novel inversion approach and conclusions about the Iberian Peninsula subsurface,<br />

together with suggestions for future work (Chapter 11). This summary is followed by the<br />

Appendix containing auxiliary information that were moved to the end of this thesis, for<br />

the sake of clarity in the main body (Chapter A). Sections in this Appendix comprise a<br />

detailed study of the Iberian Peninsula evolution (Section A.1), specific aspects of MT<br />

inversion related to this thesis work (Section A.2), and a detailed examination of results<br />

from the synthetic model study (Section A.3), as well as a comparison of response curves<br />

from the PICASSO Phase I stations and from the derived subsurface models. The list<br />

of references referred to in this thesis is given at the end of this body of work (Chapter<br />

Bibliography).<br />

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