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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| Vydáno v: | Boletín de Geología |
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| Hlavní autoři: | , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Universidad Industrial de Santander
2021
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| Témata: | |
| On-line přístup: | 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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