Biostratigraphy and paleoecology of the upper Miocene (Messinian) and lower Pliocene(?) Cerro de Almendral section, Almeria Basin, southern Spain

1981 ◽  
Author(s):  
R.Z. Poore ◽  
S.M. Stone
Keyword(s):  
Southern Spain ◽  
Upper Miocene

Micromammal biostratigraphy of the Upper Miocene to lowest Pleistocene continental deposits of the Guadix basin, southern Spain

Lethaia ◽  
2012 ◽  
Vol 45 (4) ◽  
pp. 594-614 ◽  
Author(s):  
RAEF MINWER-BARAKAT ◽  
ANTONIO GARCÍA-ALIX ◽  
ELVIRA MARTÍN SUÁREZ ◽  
MATTHIJS FREUDENTHAL ◽  
CÉSAR VISERAS
Keyword(s):  
Southern Spain ◽  
Upper Miocene ◽  
Continental Deposits

Sedimentological and ichnological signatures of an offshore-transitional hyperpycnal system (Upper Miocene, Betic Cordillera, southern Spain)

2021 ◽  
Vol 561 ◽  
pp. 110039
Author(s):  
F. García-García ◽  
F.J. Rodríguez-Tovar ◽  
M. Poyatos-Moré ◽  
L.M. Yeste ◽  
C. Viseras
Keyword(s):  
Betic Cordillera ◽  
Southern Spain ◽  
Upper Miocene

Relationships between oblique convergence partitioning and plate kinematics. A case study from the western Betics external zones and foreland (southern Spain)

2020 ◽  
Author(s):  
Manuel Díaz-Azpiroz ◽  
Inmaculada Expósito ◽  
Alejandro Jiménez-Bonilla ◽  
Juan Carlos Balanyá
Keyword(s):  
Foreland Basin ◽  
Strike Slip ◽  
Southern Spain ◽  
Thrust Belt ◽  
Strain Partitioning ◽  
Seismic Profiles ◽  
Tectonic Plates ◽  
Upper Miocene ◽  
Fold And Thrust Belt ◽  
Oblique Convergence

<p>Displacement between tectonic plates is normally partitioned into different tectonic domains accommodating specific components of the bulk strain, such that no single domain can possibly be regarded as representative of the overall kinematics. Eventually, this partitioning can be produced at different scales. Therefore, plate kinematic motion estimations based on the surface geological record should ideally rely on detailed multiscale, structural analyses of all different tectonic domains involved.</p><p>The Betic-Rif orogen was formed during the Cenozoic by the convergence and subsequent collision of the Alboran domain and the South Iberian and Maghrebian paleomargins. After the main Miocene event, oblique convergence has been still active up to present times in both branches of the resulting Gibraltar Arc. In this work we analyze how dextral oblique convergence in the northern Betic branch is partitioned into different tectonic domains of the orogen external zones and foreland, where contrasting strain fields are deduced. These domains present distinctive rheologies, thus showing also specific structural styles. As such, we present data of upper Miocene-Present structures from four different tectonic domains along a complete transect of the western Betics (southern Spain), from the internal-external zones boundary outwards. In the inner fold and thrust belt, the detached South Iberian paleomargin and Flysch trough units (mostly limestones and other carbonatic rocks) are deformed mainly by upright and double-verging folds as well as reverse faults, both registering mostly orthogonal shortening. The outer fold and thrust belt progressed toward the foreland incorporating block-in-matrix formations, with evaporite-rich marly matrix, formed ahead the mountain front; its main deformation is resolved at a strike-slip dominated, dextral transpressional zone. The upper Miocene deposits of the foreland basin (calcarenites and marls) are affected by weak deformation combining some shortening and an unconstrained strike-slip component, as deduced from seismic profiles. Finally, Paleozoic structures of the foreland, formerly developed at non- to medium-grade metamorphic conditions, were likely reactivated under a dextral transpressional strain field, which acts in combination with forebulge bending.</p><p>The strongly arcuate shape of the Gibraltar Arc likely imposes contrasting kinematics along strike within the same tectonic domain. Indeed, the inner fold and thrust belt shows nearly orthogonal shortening to the west, in a more frontal position, and a strike-slip dominated high-strain zone (the so-called Torcal shear zone) to the east. By contrast, preliminary studies show no significant differences in the kinematics of the foreland eastward from the analyzed transect.</p><p>All of our kinematic results from the studied domains are compatible with an overall dextral oblique convergence. However, more accurate strain estimations are needed to constrain the plate displacements responsible for the upper Miocene-Recent deformation in the Gibraltar Arc northern branch. Moreover, detailed analyses of strain partitioning modes will shed light into the relationships between these plate displacements and the resulting strain patterns.</p>

Petrochemical characterization of the upper Miocene Rodna-Bârgău subvolcanic district (Eastern Carpathians)

2016 ◽  
Vol 39 ◽  
pp. 142-145
Author(s):  
Fabio Laiena ◽  
Lorenzo Fedele ◽  
Ioan Seghedi ◽  
Vincenzo Morra
Keyword(s):  
Upper Miocene ◽  
Eastern Carpathians
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