Utilizza questo identificativo per citare o creare un link a questo documento: http://dx.doi.org/10.15165/studgeocam-1456
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dc.contributor.authorGUARNIERI, P.-
dc.date.accessioned2018-01-17T10:12:46Z-
dc.date.available2018-01-17T10:12:46Z-
dc.date.issued2003-
dc.identifier.citationStudi geologici camerti. Nuova serie, 2003/1, pp.69-80 + 1 cartait
dc.identifier.issn1827-1979-
dc.identifier.urihttp://193.204.8.201:8080/jspui/handle/1336/833-
dc.description.abstractThe present paper considers the geology of the mountain range around Termini Imerese in northwestern Sicily. Much strati­graphical and structural work has been carried out in this area of the Apenninic-Maghrebian chain in the past, which has resulted in a generai description of its geologica! evolution and, most of all, a characterization of the sedimentary sequences. During the past decade the framework of the neotectonic evolution of both eastem and western Sicily has evolved notably thanks to severa! syntheti­zing publications on a regional scale, which are based on a vast amount of geologica! data derived from the interpretation of sei­smic lines recorded on land and in the Tyrrhenian offshore. These works have revealed new structural elements and opened the way toward a modem vision of the geology of Sicily. [...]it
dc.publisherUniversità di Camerinoit
dc.subjectStructural Geology - Transpressive tectonics - Sicily - Neogeneit
dc.subjectGeologia strutturale - tettonica traspressiva - Sicilia - Neogeneit
dc.titleSTRUCTURAL FEATURES OF THE TRABIA-TERMINI IMERESE MOUNTAIN BELT (NW-SICILY)en
dc.title.alternativeLineamenti strutturali dei Monti di Trabia-Termini Imerese (Sicilia nord-occidentale)it
dc.description.pages69-80 + 1 carta-
dc.identifier.sequenza6it
dc.identifier.capitolo6it
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