© 2015, Swiss Geological Society. The existence of an orogenic arc in the Variscan belt of Central Iberia is traced from its first recognition by the Swiss geologist, Rudolf Staub, at the XIV International Geological Congress (Madrid 1926), to the present. A review of the literature exposes the main facts related to Staub’s original interpretation, and its subsequent discussion, rejection and rehabilitation in the 21st century. The “Castilian bend” or Central Iberian arc is defined as a secondary orocline formed during late stages of the Variscan orogeny, with a curvature opposite to that of the better known Ibero-Armorican arc. It bends the older Variscan, structures, the magnetic anomalies, and the stratigraphic, metamorphic, and magmatic zonation of the Iberian Massif. The original NE–SW trend of these elements has been preserved by porphyroblast inclusion trails that maintained constant orientations during the formation of both oroclines. The rediscovery of the Central Iberian arc has given a new impulse to research in the Iberian Massif during the last decade, which we briefly review. A short discussion is also included of remaining unknowns regarding the precise geometry and formation mechanism of the arc, and the new perspectives it opens for future research in the Variscan belt.
|Journal||Swiss Journal of Geosciences|
|Publication status||Published - 1 Dec 2015|
- Central Iberian arc
- Curved orogens
- Iberian Massif
- Variscan belt