The Santa Maria de Alameda (Madrid) Ductile Shear Zone is a complex mylonitic belt trending east -West and dipping 30°-60° southward. The hanging wall block sinks towards the South-Southeast. Its kinematics is in relation to an extensional tectonic regime with North-south stretching direction. This large structure belongs to the early stages of the Malagon tectonic period, where important faulting and dike emplacement were produced. The shearing process was developed in retrograde metamorphic conditions in a wide range of temperature, which goes from 400° C to 150° C. The age of this deformation is constrained by the variscan regional metamorphic peak and the intrusion of late variscan granitoids (Las Navas del Marques adamellites), being t...
A composite cross section from the Florianópolis Batholith towards the Tijucas Fold Belt in the nort...
Variscan deformation in the Badajoz-Códoba Shear Zone, a long-lived tectonic lineament in SW Iberia,...
The exhumation mechanisms of deep-seated continental crust can be constrained by analyzing the struc...
The tectonothermal Variscan evolution of the Tormes Gneiss Dome is controlled by a subhorizontal duc...
We describe the main features of the Campillo shear zone, a band of intense deformation made of mylo...
The Sierra Ballena Shear Zone (SBSZ) is part of a high-strain transcurrent system that divides the N...
The existence in the Alpujarride Complex (Betic Cordillera, southern Spain) of a relatively continuo...
The Los Llanos Shear Zone bounds the Cabeza Gorda and Zafra units located in the Ossa-Morena Zone (...
In this paper, a new structural analysis of the Somosierra sector of the Spanish Central System is p...
The existence in the Alpujarride Complex (Betic Cordillera, southern Spain) of a relatively continuo...
Evidence of a late-metamorphic extensional shear activity has been found along the central part of t...
Shear with SC planes are found in the same locations among the gneises and other metamorphic rocks i...
The La Codosera area is located within the Central Iberian Zone just to the north of the Badajoz-Cor...
The Coimbra-Cordoba shear zone (Iberian Massif), characterized by simple-shear dominated sinistral t...
An extensional britt/e detachment with a top-to-the-west directed movement exists between the Alpujá...
A composite cross section from the Florianópolis Batholith towards the Tijucas Fold Belt in the nort...
Variscan deformation in the Badajoz-Códoba Shear Zone, a long-lived tectonic lineament in SW Iberia,...
The exhumation mechanisms of deep-seated continental crust can be constrained by analyzing the struc...
The tectonothermal Variscan evolution of the Tormes Gneiss Dome is controlled by a subhorizontal duc...
We describe the main features of the Campillo shear zone, a band of intense deformation made of mylo...
The Sierra Ballena Shear Zone (SBSZ) is part of a high-strain transcurrent system that divides the N...
The existence in the Alpujarride Complex (Betic Cordillera, southern Spain) of a relatively continuo...
The Los Llanos Shear Zone bounds the Cabeza Gorda and Zafra units located in the Ossa-Morena Zone (...
In this paper, a new structural analysis of the Somosierra sector of the Spanish Central System is p...
The existence in the Alpujarride Complex (Betic Cordillera, southern Spain) of a relatively continuo...
Evidence of a late-metamorphic extensional shear activity has been found along the central part of t...
Shear with SC planes are found in the same locations among the gneises and other metamorphic rocks i...
The La Codosera area is located within the Central Iberian Zone just to the north of the Badajoz-Cor...
The Coimbra-Cordoba shear zone (Iberian Massif), characterized by simple-shear dominated sinistral t...
An extensional britt/e detachment with a top-to-the-west directed movement exists between the Alpujá...
A composite cross section from the Florianópolis Batholith towards the Tijucas Fold Belt in the nort...
Variscan deformation in the Badajoz-Códoba Shear Zone, a long-lived tectonic lineament in SW Iberia,...
The exhumation mechanisms of deep-seated continental crust can be constrained by analyzing the struc...
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