Insights of active extension within a collisional orogen from GNSS (Central Betic Cordillera, S Spain)
The coexistence of shortening and extensional tectonic regimes is a common feature in
orogenic belts. The westernmost end of the Western Mediterranean is an area undergoing …
orogenic belts. The westernmost end of the Western Mediterranean is an area undergoing …
Active collapse in the central Betic Cordillera: Development of the extensional system of the Granada Basin
The Betic Cordillera was formed by the collision between the Alboran Domain and the South
Iberian paleomargin in the frame of the NW–SE convergent Eurasia–Nubia plate boundary …
Iberian paleomargin in the frame of the NW–SE convergent Eurasia–Nubia plate boundary …
Topo-Iberia CGPS network: a new 3D crustal velocity field in the Iberian Peninsula and Morocco based on 11 years (2008–2019)
JA García-Armenteros - GPS Solutions, 2023 - Springer
Abstract The Topo-Iberia network covering the Spanish part of the Iberian Peninsula and
Morocco was established in 2008. Following the first publication of the horizontal velocity …
Morocco was established in 2008. Following the first publication of the horizontal velocity …
Deterministic seismic hazard assessment of the area comprised between west Gulf of Cádiz and east Alboran Sea
AJ Rosario Beltré… - … Hazards and Earth …, 2023 - nhess.copernicus.org
The convergence zone of the NE-SW complex comprising the Gulf of Cádiz and the Alboran
Sea, at the Eurasian-Nubian plate boundary, is frequently affected by seismic activity …
Sea, at the Eurasian-Nubian plate boundary, is frequently affected by seismic activity …
Active shortening simultaneous to normal faulting based on GNSS, geophysical, and geological data: The seismogenic Ventas de Zafarraya Fault (Betic Cordillera …
A Madarieta‐Txurruka, L González‐Castillo… - …, 2024 - Wiley Online Library
Abstract The central Betic Cordillera, southern Spain, is affected by an uplift related to the
NNW–SSE Eurasia‐Nubia convergence and shallow ENE–WSW orthogonal extension …
NNW–SSE Eurasia‐Nubia convergence and shallow ENE–WSW orthogonal extension …
Gravimetric survey and modelling of a tectonic indenter boundary: The Palomares Fault Zone (Betic Cordillera, Iberia)
V Tendero-Salmerón, G Ercilla, L González-Castillo… - Tectonophysics, 2024 - Elsevier
New gravimetric data are improving our understanding of the Palomares Fault Zone (PFZ)
that accommodates the Águilas Arc tectonic indentation (eastern Betic Cordillera, SE Iberia) …
that accommodates the Águilas Arc tectonic indentation (eastern Betic Cordillera, SE Iberia) …
Unveiling the potential of karst vadose deposits in constraining Quaternary tectonic subsidence
D Ballesteros, C Pérez‐Mejías… - Earth Surface …, 2024 - Wiley Online Library
In carbonate coastlines, karst studies have traditionally focused on reconstructing
Quaternary coastal uplift and sea level oscillations. However, their potential for investigating …
Quaternary coastal uplift and sea level oscillations. However, their potential for investigating …
[HTML][HTML] Azimuthal seismic anisotropy in the crust beneath the Granada Basin (Spain)
I Serrano, MA Dengra, F Torcal, D Zhao - Tectonophysics, 2024 - Elsevier
In this research, we conducted the first P-wave tomographic imaging of 3-D azimuthal
anisotropy of the Granada Basin (Betic Cordillera, Spain) introducing recent advances in the …
anisotropy of the Granada Basin (Betic Cordillera, Spain) introducing recent advances in the …
Azimuthal seismic anisotropy in the crust beneath the Granada Basin (Spain)
I Serrano Bermejo, MÁ Dengra Martínez… - 2024 - digibug.ugr.es
In this research, we conducted the first P-wave tomographic imaging of 3-D azimuthal
anisotropy of the Granada Basin (Betic Cordillera, Spain) introducing recent advances in the …
anisotropy of the Granada Basin (Betic Cordillera, Spain) introducing recent advances in the …
Active Collapse in the Central Betic Cordillera: Development of the Extensional System of the Granada Basin
M Txurruka, ML González Castillo, J Galindo Zaldívar - 2023 - digibug.ugr.es
The Betic Cordillera was formed by the collision between the Alboran Domain and the South
Iberian paleomargin in the frame of the NW–SE convergent Eurasia–Nubia plate boundary …
Iberian paleomargin in the frame of the NW–SE convergent Eurasia–Nubia plate boundary …