Utilizza questo identificativo per citare o creare un link a questo documento: http://dx.doi.org/10.15165/studgeocam-1326
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Campo DCValoreLingua
dc.contributor.authorPICCARDI, L.-
dc.contributor.authorMORATTI, G.-
dc.contributor.authorVANNUCCI, G.-
dc.contributor.authorBENDKIK, A.-
dc.contributor.authorCHENAKEB, M.-
dc.date.accessioned2017-12-05T09:34:37Z-
dc.date.available2017-12-05T09:34:37Z-
dc.date.issued2004-
dc.identifier.citationStudi geologici camerti, n. speciale, 2004, pp. 123-127it
dc.identifier.issn0392-0631-
dc.identifier.urihttp://193.204.8.201:8080/jspui/handle/1336/691-
dc.description.abstractThe November 1 st, 1755 Lisbon earthquake has been largely studied, its source constrained to be a 200 km long structure, its magnitude estimated around 8 .7, and the stress regime argued as a NNW-SSE directed compression. Less well known is the Meknes earthquake, occurred a few days later in Morocco and considered the effect of a strong aftershock in Portugal. [...]en
dc.publisherUniversità di Camerinoit
dc.subjectSeismotectonics - surface rupture - earthquake - Rides Prérifainesen
dc.titleSEISMOTECTONICS OF THE 1755 MEKNES EARTHQUAKE (MOROCCO)en
dc.description.pages123-127-
E' visualizzato nelle collezioni:2004: Proceeding of the workshop COST-ACTION 625 "Active fault: analysis processes and monitoring", Camerino, Italy, May 3-6 2002

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