Please use this identifier to cite or link to this item: http://dx.doi.org/10.15165/studgeocam-1219
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dc.contributor.authorDECANDIA, F. A.-
dc.contributor.authorTAVARNELLI, E.-
dc.date.accessioned2017-11-09T09:58:50Z-
dc.date.available2017-11-09T09:58:50Z-
dc.date.issued1991-
dc.identifier.citationStudi geologici camerti, n. speciale, 1991, pp. 329-330it
dc.identifier.issn0392-0631-
dc.identifier.urihttp://193.204.8.201:8080/jspui/handle/1336/571-
dc.description.abstractCompressional tectonics in Umbria-Marche Apennines are expressed by the superimposition of structures originated during two main deformational events, which occurred respec­tivel y during Tortonian and Messinian.it
dc.publisherUniversità di Camerinoit
dc.subjectUmbria sud-orientale - Fasi tettoniche compressiveit
dc.subjectSouth-eastern Umbria - Compressional tectonic phasesit
dc.titleCRONOLOGIA DELLE DEFORMAZIONI NELL'AREA DI SPOLETO (UMBRIA SUD-ORIENTALE)it
dc.description.pages329-330-
dc.identifier.sequenza33-
Appears in Volumess:1991/1: "Studi preliminari all'acquisizione dati del profilo CROP 03 Punta Ala-Gabicce"

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