An array of 200-Ma-old (Lower Jurassic) dolerite dikes in both the eastern and western sides of the Atlantic records an episode of SE directed extension which occurred in and around the Iberian Peninsula. This extensional regime episode is responsible for the formation of the main structures in the Iberian Peninsula and neighboring areas at the beginning of the JurassicUna serie de diques básicos de edad Jurásico Inferior (200 Ma), tanto en las zonas orientales como occidentales del dominio Atlántico, permite definir un episodio de extensión con dirección SE que afectó a la Península Ibérica y a las regiones vecinas. Este episodio de régimen extensional es responsable de la formación de las principales estructuras de la Península Ibérica y ...
Iberia underwent intraplate deformation during the Mesozoic and Cenozoic. In eastem Ibena, compressi...
The Concòrdia is the grouping of outcrops of Jurassic volcanic materials located southermost of the...
The western European kinematic evolution results from the opening of the western Neotethys and the A...
An array of 200-Ma-old (Lower Jurassic) dolerite dikes in both the eastern and western sides of the ...
The Plasencia dike belongs to a vast Early Jurassic magmatic province that extends around the Centra...
Deposition of Upper Triassic and Lower Jurassic sediments on the Iberian platform system took place ...
A dense grid of multichannel (2D) seismic profiles, tied to borehole, dredge and outcrop data are us...
The Ligurian Tethys began to open in a roughly NE–SW direction in Pliensbachian times. West of the L...
International audienceThe western European kinematic evolution results from the opening of the weste...
Facies analysis and geological mapping of the Triassic-Jurassic transition units (Cor tes de Tajuña ...
Regional (2-D) seismic reflection profiles, outcrop, and borehole data are used to characterize the ...
Iberia underwent intraplate deformation during the Mesozoic and Cenozoic. In eastem Ibena, compressi...
The Concòrdia is the grouping of outcrops of Jurassic volcanic materials located southermost of the...
The western European kinematic evolution results from the opening of the western Neotethys and the A...
An array of 200-Ma-old (Lower Jurassic) dolerite dikes in both the eastern and western sides of the ...
The Plasencia dike belongs to a vast Early Jurassic magmatic province that extends around the Centra...
Deposition of Upper Triassic and Lower Jurassic sediments on the Iberian platform system took place ...
A dense grid of multichannel (2D) seismic profiles, tied to borehole, dredge and outcrop data are us...
The Ligurian Tethys began to open in a roughly NE–SW direction in Pliensbachian times. West of the L...
International audienceThe western European kinematic evolution results from the opening of the weste...
Facies analysis and geological mapping of the Triassic-Jurassic transition units (Cor tes de Tajuña ...
Regional (2-D) seismic reflection profiles, outcrop, and borehole data are used to characterize the ...
Iberia underwent intraplate deformation during the Mesozoic and Cenozoic. In eastem Ibena, compressi...
The Concòrdia is the grouping of outcrops of Jurassic volcanic materials located southermost of the...
The western European kinematic evolution results from the opening of the western Neotethys and the A...