Evidence for quaternary seismic activity of the La Alberca-Teremendo fault, Morelia region, Trans-Mexican Volcanic Belt
The La Alberca-Teremendo fault is a 26 km-long, complex fault composed of an en échelon array of short crustal fault segments, belonging to the Morelia-Acambay fault system. This fault system shows parallel scarps with morphological evidence of recent activity such as drainage alteration, maximum th...
Shranjeno v:
| izdano v: | Revista Mexicana de Ciencias Geológicas |
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| Principais autores: | , , , , |
| Format: | Artigo |
| Jezik: | Inglês |
| Izdano: |
Universidad Nacional Autónoma de México
2019
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| Teme: | |
| Online dostop: | https://www.redalyc.org/articulo.oa?id=57265251008 https://www.redalyc.org/journal/572/57265251008/ https://www.redalyc.org/journal/572/57265251008/html/ https://www.redalyc.org/journal/572/57265251008/57265251008.epub https://www.redalyc.org/journal/572/57265251008/movil |
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