PALEOSEISMOLOGY ANALYSIS ALONG THE MATTINATA FAULT, APULIA FOREL AND, SOUTHERN ITALY

Utilizza questo identificativo per citare o creare un link a questo documento: http://dx.doi.org/10.15165/studgeocam-1325

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Campo DC	Valore	Lingua
dc.contributor.author	PICCARDI, L.	-
dc.contributor.author	FERRELI, L.	-
dc.contributor.author	TONDI, E.	-
dc.contributor.author	MICHETTI, A. M.	-
dc.contributor.author	VITTORI, E.	-
dc.date.accessioned	2017-12-05T09:27:05Z	-
dc.date.available	2017-12-05T09:27:05Z	-
dc.date.issued	2004	-
dc.identifier.citation	Studi geologici camerti, n. speciale, 2004, pp. 119-122	it
dc.identifier.issn	0392-0631	-
dc.identifier.uri	http://193.204.8.201:8080/jspui/handle/1336/690	-
dc.description.abstract	Paleoseismic analyses have been carried out in a segment of the South Gargano Line (SGL), east-west-trending, right-lateral strike-slip structure, that cuts through the southern side of the Gargano promontory, a carbonate massif belonging to the Adria rnicroplate, the foreland of both the Apenninic and Dinaric mountain chains. The SGL is a seismogenic structure, with an historic earthquake in 1627 in its western segment reaching Imax=X MCS. However, the knowledge on the local seisrnicity is still limited. [...]	en
dc.publisher	Università di Camerino	it
dc.subject	Active fault - slip rate - radiocarbon dating	en
dc.title	PALEOSEISMOLOGY ANALYSIS ALONG THE MATTINATA FAULT, APULIA FOREL AND, SOUTHERN ITALY	en
dc.description.pages	119-122	-
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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STUDI GEOLOGICI CAMERTI