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Ana Crespo-Blanc

Researcher at University of Granada

Publications -  38
Citations -  2560

Ana Crespo-Blanc is an academic researcher from University of Granada. The author has contributed to research in topics: Flysch & Subduction. The author has an hindex of 22, co-authored 37 publications receiving 2348 citations. Previous affiliations of Ana Crespo-Blanc include University of Seville & Spanish National Research Council.

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Lateral slab deformation and the origin of the western Mediterranean arcs

TL;DR: In this article, the authors describe the evolution of the western Mediterranean subduction zone (WMSZ) during the last 35 Myr by combining new and previous geological data, new tomographic images of the Western Mediterranean mantle, and plate kinematics.
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Subduction, convergence and the mode of backarc extension in the Mediterranean region

TL;DR: In this paper, the authors show that the sense of shear along crustal-scale detachments is toward the trench when subduction proceeds with little or no convergence and away from the trench in the case of true convergence (Aegean).
Journal Article

Subduction convergence and the mode of backarc extension in the Mediterranean region

TL;DR: In this paper, the authors show that the sense of shear along crustal-scale detachments is toward the trench when subduction proceeds with little or no convergence and away from the trench in the case of true convergence (Aegean).
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Extension versus compression during the Miocene tectonic evolution of the Betic chain. Late folding of normal fault systems

TL;DR: In this article, the authors studied the cortical segment formed the basement of the Miocene Alboran Basin, in which progressively deeper basement units were covered by younger marine sediments as a result of extensional denudation processes.
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Exhumation during a continental collision inferred from the tectonometamorphic evolution of the Alpujarride Complex in the central Betics (Alboran Domain, SE Spain)

J.M. Azañón, +1 more
- 01 Jun 2000 - 
TL;DR: In this article, a complex tectonometamorphic evolution of the Alpujarride Complex within the internal zones of the Betics reveals a complex structural and metamorphic succession of continental collision, synmetamorphic exhumation, nappe forming in the final stage, and rifting.