The major Al Medinat fault; an Atlasic reworking of a complex Variscan shear zones system (western High Atlas, Morocco)
The geological pattern of Morocco is the result of a strong interference between several orogenic cycles from the Precambrian to recent times, which led to the individualization of different tectonic domains. Their boundaries are mostly the result of brittle deformation, induced by the Cainozoic com...
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| Formato: | lecture |
| Idioma: | eng |
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2018
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| Texto completo: | http://hdl.handle.net/10174/22926 |
| País: | Portugal |
| Oai: | oai:dspace.uevora.pt:10174/22926 |