Strain partitioning in the Variscan deformation of the Marão domain (Central Iberian zone; northern Portugal)
formation of the Ibero-Armorican Arc, a major structure in the SW Variscan orogeny, induced in most of its southern Iberian branch a heterogeneous sinistral transpressive regime. The presence of pre- and syn-orogenic steep planar anisotropies subparallel to the main WNW-ESE structural trend, gave ri...
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| Other Authors: | , |
| Format: | article |
| Language: | por |
| Published: |
2022
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| Subjects: | |
| Online Access: | http://hdl.handle.net/10174/32877 http://hdl.handle.net/10174/32877 |
| Country: | Portugal |
| Oai: | oai:dspace.uevora.pt:10174/32877 |