Geological aspects of paleoseismicity and archaeosismology in the fluvial alluvial Rimac valley
The sedimentary fill of the Rimac River fluvial-alluvial plain (Upper Miocene-Quaternary) consists of a thick sequence of unconsolidated material that corresponds to fluvial deposits. A record of seismotectonic activity is presentedin the sedimentary levels of fine facie within numerous paleoseismic...
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Format: | Others |
Language: | Español |
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Pontificia Universidad Católica del Perú
2017
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Online Access: | http://revistas.pucp.edu.pe/index.php/boletindearqueologia/article/view/16618/16955 http://repositorio.pucp.edu.pe/index/handle/123456789/113495 |