Soft-sediment deformation structures induced by seismic activity in the San Pedro el Alto area, Acambay graben, Mexico
Soft-sediment deformation structures identified in lacustrine sediments of the San Pedro el Alto area, within the Acambay graben, Mexico, can be attributed to Pleistocene-Holocene seismic events. The analysis of these deformation structures, seismites, is a key tool for the characterization of param...
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| Vydáno v: | Revista Mexicana de Ciencias Geológicas |
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| Hlavní autoři: | , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Universidad Nacional Autónoma de México
2018
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| Témata: | |
| On-line přístup: | https://www.redalyc.org/articulo.oa?id=57265254003 https://www.redalyc.org/journal/572/57265254003/ https://www.redalyc.org/journal/572/57265254003/html/ https://www.redalyc.org/journal/572/57265254003/57265254003.epub https://www.redalyc.org/journal/572/57265254003/movil https://doi.org/10.22201/cgeo.20072902e.2018.1.530 |
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