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Phase-transformation-induced lubrication of earthquake sliding

Frictional failure is not possible at depth in Earth, hence earthquakes deeper than 30–50 km cannot initiate by overcoming dry friction. Moreover, the frequency distribution of earthquakes with depth is bimodal, suggesting another change of mechanism at about 350 km. Here I suggest that the change a...

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Bibliografiske detaljer
Udgivet i:Philos Trans A Math Phys Eng Sci
Hovedforfatter: Green, Harry W.
Format: Artigo
Sprog:Inglês
Udgivet: The Royal Society Publishing 2017
Fag:
Online adgang:https://ncbi.nlm.nih.gov/pmc/articles/PMC5580448/
https://ncbi.nlm.nih.gov/pubmed/28827426
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rsta.2016.0008
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