scholarly journals Influence of rift basin geometry on the subsequent postrift sedimentation and basin inversion: The Organyà Basin and the Bóixols thrust sheet (south central Pyrenees)

Tectonics ◽  
2015 ◽  
Vol 34 (7) ◽  
pp. 1452-1474 ◽  
Author(s):  
Joana Mencos ◽  
Núria Carrera ◽  
Josep Anton Muñoz
Keyword(s):  
Rift Basin ◽  
Thrust Sheet ◽  
Basin Inversion ◽  
South Central ◽  
Basin Geometry ◽  
Central Pyrenees

Palynological characterization of a transgressive episode in transitional deposits in the Cretaceous Aren and Tremp formations (south-central Pyrenees, Spain)

2012 ◽  
Vol 266 (2) ◽  
pp. 159-172 ◽  
Author(s):  
Angélica Torices ◽  
María-Teresa Fernández-Marrón ◽  
Fernando Fonollá ◽  
Nieves López-Martínez
Keyword(s):  
South Central ◽  
Central Pyrenees

scholarly journals Tectonic control on sediment sources in the Jaca basin (Middle and Upper Eocene of the South-Central Pyrenees)

2016 ◽  
Vol 348 (3-4) ◽  
pp. 236-245 ◽  
Author(s):  
Marta Roigé ◽  
David Gómez-Gras ◽  
Eduard Remacha ◽  
Raquel Daza ◽  
Salvador Boya
Keyword(s):  
Upper Eocene ◽  
Sediment Sources ◽  
The South ◽  
Tectonic Control ◽  
South Central ◽  
Central Pyrenees

scholarly journals Multiple fluid flow events from salt‐related rifting to basin inversion (Upper Pedraforca thrust sheet, SE Pyrenees)

2021 ◽  
Author(s):  
David Cruset ◽  
Jaume Vergés ◽  
Antonio Benedicto ◽  
Enrique Gomez‐Rivas ◽  
Irene Cantarero ◽  
...  
Keyword(s):  
Fluid Flow ◽  
Thrust Sheet ◽  
Basin Inversion

scholarly journals 3D reconstruction of syn-tectonic strata in a salt-related orogen: learnings from the Llert syncline (South-central Pyrenees)

2020 ◽  
Vol 18 ◽  
pp. 1-19
Author(s):  
Adrià Ramos ◽  
Berta Lopez-Mir ◽  
Elisabeth P. Wilson ◽  
Pablo Granado ◽  
Josep Anton Muñoz
Keyword(s):  
3D Reconstruction ◽  
Field Research ◽  
Rift System ◽  
Passive Margins ◽  
Fold System ◽  
The North ◽  
Structural Framework ◽  
South Central ◽  
Insight Into ◽  
Central Pyrenees

The Llert syncline is located in the South-central Pyrenees, between the eastern termination of the EW-trending Cotiella Basin and the north-western limb of the NS-trending Turbón-Serrado fold system. The Cotiella Basin is an inverted upper Coniacian-lower Santonian salt-floored post-rift extensional basin developed along the northern Iberian rift system. The Turbón-Serrado fold system consists of upper Santonian – Maastrichtian contractional salt-cored anticlines developed along an inverted transfer zone of the Pyrenean rift system. Based on field research, this paper presents a 3D reconstruction of the Llert syncline in order to further constrain the transition between these oblique salt-related structures. Our results suggest that the evolution of the Llert syncline was mainly controlled by tectonic shortening related to the tectonic inversion of the Cotiella Basin synchronously to the growth of the Turbón-Serrado detachment anticline, and by the pre-compressional structural framework of the Pyrenean rift system. Our contribution provides new insight into the geometric and kinematic relationships of structures developed during the inversion of passive margins involving salt.

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