Structural changes caused by dips in lateral ramps of fold and thrust belts
Transverse zones are tectonic structures parallel or oblique to the shortening direction. Lateral ramps are inherited tectonic structures and are comprised in a transverse zone. During shortening transverse zones are usually confused with simple strike-slip faults. We evaluated 36 analogue models un...
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| Publicado no: | Boletín de Geología |
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| Principais autores: | , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Universidad Industrial de Santander
2021
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| Assuntos: | |
| Acesso em linha: | https://www.redalyc.org/articulo.oa?id=349670461002 https://www.redalyc.org/journal/3496/349670461002/ https://www.redalyc.org/journal/3496/349670461002/html/ https://www.redalyc.org/journal/3496/349670461002/349670461002.epub https://www.redalyc.org/journal/3496/349670461002/movil |
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