Sand blows formed after the 2012 Emilia earthquake in Italy, indicating
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Download scientific diagram | Sand blows formed after the 2012 Emilia earthquake in Italy, indicating pore-water escape and liquefaction/luidization, which must have resulted in the formation of SSDS of a buried layer, which consequently should be considered as a seismite (from Emergeo Working Group, 2012). from publication: Restrictions to the application of ‘diagnostic’ criteria for recognizing ancient seismites | Soft-sediment deformation structures induced by seismic liquefaction and/or fluidization receive much attention in sedimentological, structural and palaeoseismic studies. The direct record of larger earthquakes is restricted to instrumental and historical data; the | Congenital Abnormalities, Seismics and Restriction | ResearchGate, the professional network for scientists.
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