The Cantabrian orocline is a large structure that bends the Variscan orogen of Western Europe in NW Iberia. The extensively studied kinematics of its core, the foreland of the orogen, indicates that the structure is secondary, i.e. acquired after the formation of the orogenic edifice. However, the extent of the Cantabrian orocline away from its core is under debate. In this paper we study the kinematics of the Cantabrian orocline beyond the foreland. We collected and analyzed samples from the northern and central parts of the Truchas syncline, which provides new data within the hinterland of the orogen in NW Iberia. The analysis of 320 samples shows a late Carboniferous remagnetization with an E to NE declination and shallow downward inclin...
[EN] A magnetic and paleomagnetic study was carried out on weakly metamorphic Cambrian limestones fr...
Supercontinents are usually interpreted to be single and rigid continental plates. How and when Pang...
Supercontinents are usually interpreted to be single and rigid continental plates. How and when Pang...
The Cantabrian orocline is a large structure that bends the Variscan orogen of Western Europe in NW ...
The Variscan mountain belt in Iberia defines a large “S” shape with the Cantabrian Orocline in the n...
The Variscan mountain belt in Iberia defines a large “S” shape with the Cantabrian Orocline in the n...
The Variscan mountain belt in Iberia defines a large “S” shape with the Cantabrian Orocline in the n...
The Variscan Belt in Iberia forms an “S” shape double orocline. The northern orocline, the Cantabria...
The amalgamation of Pangea formed the contorted Variscan-Alleghanian orogen, suturing Gondwana and L...
The amalgamation of Pangea formed the contorted Variscan-Alleghanian orogen, suturing Gondwana and L...
The amalgamation of Pangea formed the contorted Variscan-Alleghanian orogen, suturing Gondwana and L...
The Cantabria-Asturias Arc (CAA) of SW Europe is a highly curved Variscan belt that formed along the...
The supercontinent Pangea formed in the late Carboniferous as a result of the Gondwana- Laurussia co...
[EN] A magnetic and paleomagnetic study was carried out on weakly metamorphic Cambrian limestones fr...
[EN] A magnetic and paleomagnetic study was carried out on weakly metamorphic Cambrian limestones fr...
[EN] A magnetic and paleomagnetic study was carried out on weakly metamorphic Cambrian limestones fr...
Supercontinents are usually interpreted to be single and rigid continental plates. How and when Pang...
Supercontinents are usually interpreted to be single and rigid continental plates. How and when Pang...
The Cantabrian orocline is a large structure that bends the Variscan orogen of Western Europe in NW ...
The Variscan mountain belt in Iberia defines a large “S” shape with the Cantabrian Orocline in the n...
The Variscan mountain belt in Iberia defines a large “S” shape with the Cantabrian Orocline in the n...
The Variscan mountain belt in Iberia defines a large “S” shape with the Cantabrian Orocline in the n...
The Variscan Belt in Iberia forms an “S” shape double orocline. The northern orocline, the Cantabria...
The amalgamation of Pangea formed the contorted Variscan-Alleghanian orogen, suturing Gondwana and L...
The amalgamation of Pangea formed the contorted Variscan-Alleghanian orogen, suturing Gondwana and L...
The amalgamation of Pangea formed the contorted Variscan-Alleghanian orogen, suturing Gondwana and L...
The Cantabria-Asturias Arc (CAA) of SW Europe is a highly curved Variscan belt that formed along the...
The supercontinent Pangea formed in the late Carboniferous as a result of the Gondwana- Laurussia co...
[EN] A magnetic and paleomagnetic study was carried out on weakly metamorphic Cambrian limestones fr...
[EN] A magnetic and paleomagnetic study was carried out on weakly metamorphic Cambrian limestones fr...
[EN] A magnetic and paleomagnetic study was carried out on weakly metamorphic Cambrian limestones fr...
Supercontinents are usually interpreted to be single and rigid continental plates. How and when Pang...
Supercontinents are usually interpreted to be single and rigid continental plates. How and when Pang...