Updating the marine biostratigraphy of the Granada Basin (central Betic Cordillera). Insight for the Late Miocene palaeogeographic evolution of the Atlantic – Mediterranean seaway

Geobios ◽  
2012 ◽  
Vol 45 (3) ◽  
pp. 249-263 ◽  
Author(s):  
Hugo Corbí ◽  
Carlos Lancis ◽  
Fernando García-García ◽  
José-Antonio Pina ◽  
Jesús M. Soria ◽  
...  
Keyword(s):  
Late Miocene ◽  
Betic Cordillera ◽  
Granada Basin

Late Miocene vertical movements in the Sierra Nevada and Granada Basin linking zone (Betic Cordillera, Spain): insights from marine microfossils

2017 ◽  
Vol 43 (4) ◽  
pp. 615-630 ◽  
Author(s):  
H. Corbí ◽  
J. J. Peral ◽  
F. Pérez-Valera ◽  
J. M. Soria ◽  
J. E. Tent-Manclús
Keyword(s):  
Sierra Nevada ◽  
Late Miocene ◽  
Betic Cordillera ◽  
Vertical Movements ◽  
Granada Basin

Inner structure and deformation mechanisms of normal faults in conglomerates and carbonate grainstones (Granada Basin, Betic Cordillera, Spain): Inferences on fault permeability

2012 ◽  
Vol 45 ◽  
pp. 4-20 ◽  
Author(s):  
Fabrizio Agosta ◽  
Patricia Ruano ◽  
Andrea Rustichelli ◽  
Emanuele Tondi ◽  
Jesús Galindo-Zaldívar ◽  
...  
Keyword(s):  
Betic Cordillera ◽  
Deformation Mechanisms ◽  
Normal Faults ◽  
Fault Permeability ◽  
Granada Basin

scholarly journals High‐ and low‐angle normal fault activity in a collisional orogen: The northeastern Granada Basin (Betic Cordillera)

Tectonics ◽  
2021 ◽  
Author(s):  
Asier Madarieta‐Txurruka ◽  
Jesús Galindo‐Zaldívar ◽  
Lourdes González‐Castillo ◽  
José A. Peláez ◽  
Antonio M. Ruiz‐Armenteros ◽  
...  
Keyword(s):  
Normal Fault ◽  
Betic Cordillera ◽  
Fault Activity ◽  
Collisional Orogen ◽  
Granada Basin

Biostratigraphy and sedimentary evolution of Late Miocene and Pliocene continental deposits of the Granada Basin (southern Spain)

Lethaia ◽  
2008 ◽  
Vol 41 (4) ◽  
pp. 431-446 ◽  
Author(s):  
ANTONIO GARCÍA-ALIX ◽  
RAEF MINWER-BARAKAT ◽  
JOSÉ M. MARTÍN ◽  
ELVIRA MARTÍN SUÁREZ ◽  
MATTHIJS FREUDENTHAL
Keyword(s):  
Late Miocene ◽  
Southern Spain ◽  
Sedimentary Evolution ◽  
Continental Deposits ◽  
Granada Basin

Sea cliffs resulting from late Miocene extensional tectonics: the Serra Gelada case study (Betic Cordillera, Spain)

Geomorphology ◽  
2002 ◽  
Vol 42 (3-4) ◽  
pp. 197-211 ◽  
Author(s):  
Alfonso Yébenes ◽  
Pedro Alfaro ◽  
José Delgado ◽  
Antonio Estévez ◽  
Jesús M Soria
Keyword(s):  
Late Miocene ◽  
Betic Cordillera ◽  
Extensional Tectonics ◽  
Sea Cliffs

scholarly journals Recent and present-day stresses in the Granada Basin (Betic Cordilleras): Example of a late Miocene-present-day extensional basin in a convergent plate boundary

Tectonics ◽  
1999 ◽  
Vol 18 (4) ◽  
pp. 686-702 ◽  
Author(s):  
J. Galindo-Zaldívar ◽  
A. Jabaloy ◽  
I. Serrano ◽  
J. Morales ◽  
F. González-Lodeiro ◽  
...  
Keyword(s):  
Late Miocene ◽  
Plate Boundary ◽  
Extensional Basin ◽  
Betic Cordilleras ◽  
Granada Basin

Late Miocene–Early Pliocene climatic evolution of the Granada Basin (southern Spain) deduced from the paleoecology of the micromammal associations

2008 ◽  
Vol 265 (3-4) ◽  
pp. 214-225 ◽  
Author(s):  
Antonio García-Alix ◽  
Raef Minwer-Barakat ◽  
Elvira Martín Suárez ◽  
Matthijs Freudenthal ◽  
José M. Martín
Keyword(s):  
Late Miocene ◽  
Southern Spain ◽  
Early Pliocene ◽  
Climatic Evolution ◽  
Granada Basin

scholarly journals Seismic potential of faults in the Granada basin (Betic Cordillera, Spain)

2001 ◽  
Vol 34 (4) ◽  
pp. 1595 ◽  
Author(s):  
J. A. PELAEZ MONTILLA ◽  
C. SANZ DE GALDEANO ◽  
C. LLPEZ CASADO
Keyword(s):  
Betic Cordillera ◽  
Displacement Rate ◽  
Maximum Magnitude ◽  
Empirical Relationships ◽  
Seismic Potential ◽  
Recurrence Intervals ◽  
Fault Lines ◽  
Granada Basin

A fault database has been created for the Granada basin (S Spain) concerning seismic potential in this area. The fault lines have been entered as well as their geometry and displacement rate, when known from accumulated displacement. Empirical relationships have been used between the length or surface of the faults and the maximum magnitude that they can generate. No palaeoseismic recurrence intervals are known, nor palaeoseismic estimates for displacements during earthquakes.

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