Guatemala paleoseismicity: from Late Classic Maya collapse to recent fault creep

We combine ‘on-fault’ trench observations of slip on the Polochic fault (North America-Caribbean plate boundary) with a 1200 years-long ‘near-fault’ record of seismo-turbidite generation in a lake located within 2 km of the fault. The lake record indicates that, over the past 12 centuries, 10 earthq...

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Detalles Bibliográficos
Autores principales: Brocard, Gilles, Anselmetti, Flavio S., Teyssier, Christian
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5109539/
https://www.ncbi.nlm.nih.gov/pubmed/27845383
http://dx.doi.org/10.1038/srep36976

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5109539/
https://www.ncbi.nlm.nih.gov/pubmed/27845383
http://dx.doi.org/10.1038/srep36976

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