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  1. Reviews in detail key recent advances on the geology of the Iberian Peninsula from a geodynamic perspective. Summarizes the latest studies on the record of the Cadomian, Variscan, and Alpine orogenies in Iberia. Offers readers essential insights into the evolution of plate boundaries in the western corner of Europe.

  2. Jul 31, 2023 · The inset shows a map of Europe and northern Africa with the location of the study area, marked with a red rectangle, and tectonic plate boundaries from Bird (2003), delineated with green lines. The main image is centered on the Iberian Peninsula and its continental margins and abyssal plains.

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  4. Reviews exhaustively the key recent advances on the geology of the Iberian Peninsula from a geodynamic perspective. Summarizes the latest studies on the record in Iberia of the Variscan orogeny. Maximizes the reader insights on the evolution of plate boundaries in the western corner of Europe.

  5. all over the Iberian peninsula (the so-called Iberian Meseta). These features define a landscape completely different from that of western and Mediterranean Europe and more similar to elevated areas of northern Africa and western Asia (Birot, 1959; Gladfelter, 1971; Solé Sabarís, 1978, 1983). High plains in Iberia can be classified according

  6. Sep 1, 2009 · PDF | The present-day topography of the Iberian peninsula can be considered as the result of the MesozoicCenozoic tectonic evolution of the Iberian... | Find, read and cite all the...

  7. Sep 1, 2009 · The present-day topography of the Iberian peninsula can be considered as the result of the Mesozoic–Cenozoic tectonic evolution of the Iberian plate (including rifting and basin formation during the Mesozoic and compression and mountain building processes at the borders and inner part of the plate, during the Tertiary, followed by Neogene ...

  8. Feb 16, 2018 · This is the first attempt to determine the CPD (580°C) surface (isotherm) the heat flow map and the Moho temperature map of the Iberian Peninsula with the aim of providing a view of its evolution and thermal structure.

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