Strike-slip shear zones of the Iberian Massif: Are they coeval?
Strike-slip shear zones of the Variscan orogen are used to derive the evolution of paleostrain and discuss the kinematics of the waning stages of the Gondwana-Laurussia collision during the amalgamation of Pangea. In the Iberian Massif, the recognition of three late Carboniferous deformation events...
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| Formato: | article |
| Idioma: | eng |
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2018
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| Texto completo: | http://hdl.handle.net/10174/22564 |
| País: | Portugal |
| Oai: | oai:dspace.uevora.pt:10174/22564 |