SIGLEAvailable from British Library Document Supply Centre-DSC:DXN034919 / BLDSC - British Library Document Supply CentreGBUnited Kingdo
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...
EGU General Assembly 2019, Vienna (Austria), 7-12 April, 2019The Iberian Massif is part of the...
The Subbetic Zone is an external, unmetamorphosed, thin skinned fold-and-thrust belt of Alpine age, ...
For material accompanying this thesis please apply direct to the issuing universityAvailable from Br...
The Cantabrian orocline is a large structure that bends the Variscan orogen of Western Europe in NW ...
The Cantabrian orocline is a large structure that bends the Variscan orogen of Western Europe in NW ...
X Congreso Geológico de España, 5-7 Julio 2021, Vitoria - GasteizLos niveles salinos depositados ant...
Integration of structural, stratigraphic, and paleomagnetic data from the N–S trending structures of...
[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...
The Cantabria-Asturias Arc (CAA) of SW Europe is a highly curved Variscan belt that formed along the...
The Variscan mountain belt in Iberia defines a large “S” shape with the Cantabrian Orocline in the n...
The definition of the structure and kinematics of the South-Pyrenean Frontal thrust, to the west of ...
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...
EGU General Assembly 2019, Vienna (Austria), 7-12 April, 2019The Iberian Massif is part of the...
The Subbetic Zone is an external, unmetamorphosed, thin skinned fold-and-thrust belt of Alpine age, ...
For material accompanying this thesis please apply direct to the issuing universityAvailable from Br...
The Cantabrian orocline is a large structure that bends the Variscan orogen of Western Europe in NW ...
The Cantabrian orocline is a large structure that bends the Variscan orogen of Western Europe in NW ...
X Congreso Geológico de España, 5-7 Julio 2021, Vitoria - GasteizLos niveles salinos depositados ant...
Integration of structural, stratigraphic, and paleomagnetic data from the N–S trending structures of...
[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...
The Cantabria-Asturias Arc (CAA) of SW Europe is a highly curved Variscan belt that formed along the...
The Variscan mountain belt in Iberia defines a large “S” shape with the Cantabrian Orocline in the n...
The definition of the structure and kinematics of the South-Pyrenean Frontal thrust, to the west of ...
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...
EGU General Assembly 2019, Vienna (Austria), 7-12 April, 2019The Iberian Massif is part of the...