| Autor: |
Daudet, Maxime, Mouthereau, Frédéric, Brichau, Stéphanie, Crespo‐Blanc, Ana, Gautheron, Cécile, Angrand, Paul |
| Zdroj: |
Tectonics; Jul2020, Vol. 39 Issue 7, p1-29, 29p |
| Abstrakt: |
The Betic‐Rif orogen is a key region to understand the evolution of the plate boundary between Africa and Iberia/Europe. This study focuses on the Flysch Complex, which is considered the sedimentary cover of a domain originally positioned between the Iberian and Alboran margins. Based on stratigraphic and depositional evolution constraints, evidence for salt tectonics, combined with new apatite fission‐tracks (AFT) and (U‐Th‐Sm)/He ages from the Flysch Complex and the Subbetic Zone, we propose a geodynamic interpretation for the formation of the Betic Cordillera, accounting for moderate N‐directed transport of the Flysch Complex and synchronous exhumation between External and Internal Zones of the Betic. Early contraction between Africa and Iberia/Europe is reflected in the Cretaceous Flysch basin by a prolonged period of residence in the partial annealing zone for AFT and onset of foreland subsidence at 50 Ma. This stage lasted until the Early to Middle Miocene (20–15 Ma), marked by the rapid succession, in less than 5 Ma, of the deposition of Cenozoic flysch and their rapid exhumation. This event is interpreted to reflect the W‐directed retreating mantle delamination between Africa and Iberia margins at the origin of the collapse of the proto‐Betic orogenic domain and formation of the Alboran domain. Key Points: The Flysch Complex of the Western Betic have been deposited close to their current position on the Iberian paleomarginAFT‐AHe double‐dating indicates that the Flysch Complex recorded fast heating/burial and cooling/exhumation between 20 and 15 MaTectono‐thermal evolution of the flysch deposits is consistent with proto‐Betic collision at ca. 50 Ma [ABSTRACT FROM AUTHOR] |
| Databáze: |
Complementary Index |
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