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Publikováno v:
Seismological Research Letters. 63:337-342
Earthquake-induced paleoliquefaction features are exposed in eroding river banks at 24 sites in the lower and central Wabash Valley. North-south distribution of features is at least 165 km. Sites with very large dikes (60–250 cm wide) suggestive of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3e27651fd844bdb034b35c975ca455e1
https://doi.org/10.1785/gssrl.63.3.337
https://doi.org/10.1785/gssrl.63.3.337
