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Reading a 400,000-year record of earthquake frequency for an intraplate fault

Our understanding of the frequency of large earthquakes at timescales longer than instrumental and historical records is based mostly on paleoseismic studies of fast-moving plate-boundary faults. Similar study of intraplate faults has been limited until now, because intraplate earthquake recurrence...

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Pubblicato in:Proc Natl Acad Sci U S A
Autori principali: Williams, Randolph T., Goodwin, Laurel B., Sharp, Warren D., Mozley, Peter S.
Natura: Artigo
Lingua:Inglês
Pubblicazione: National Academy of Sciences 2017
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Accesso online:https://ncbi.nlm.nih.gov/pmc/articles/PMC5441695/
https://ncbi.nlm.nih.gov/pubmed/28439002
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1617945114
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