1. Studi Geologici Camerti
  2. 2 - Studi Geologici Camerti - Volume Speciale
  3. 2004: Proceeding of the workshop COST-ACTION 625 "Active fault: analysis processes and monitoring", Camerino, Italy, May 3-6 2002
Please use this identifier to cite or link to this item: http://dx.doi.org/10.15165/studgeocam-1303
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dc.contributor.authorBENTIVENGA, M.-
dc.contributor.authorCOLTORTI, M.-
dc.contributor.authorPROSSER, G.-
dc.contributor.authorTAVARNELLI, E.-
dc.date.accessioned2017-12-04T09:16:14Z-
dc.date.available2017-12-04T09:16:14Z-
dc.date.issued2004-
dc.identifier.citationStudi geologici camerti, n. speciale, 2004, pp. 29-32it
dc.identifier.issn0392-0631-
dc.identifier.urihttp://193.204.8.201:8080/jspui/handle/1336/670-
dc.description.abstractThe front of the Southern Apennines in the Taranto Gulf is sealed by Pliocene-Pleistocene foredeep deposits, which represent the infili of the Bradanic Trough. The upper portion of the Middle Pleistocene succession consists of marine sands and conglomera­tes, that previous work considered arranged in severa! orders of ter­races. The locai drainage pattern appears controlled by prominent geomorphic lineaments [...]it
dc.publisherUniversità di Camerinoit
dc.subjectMarine terraces - normai faults - Taranto Gulfen
dc.titleMARINE TERRACES AND EXTENSIONAL FAULTING IN THE TARAN TO GULF, BRADANIC TROUGH, SOUTHERN ITALYen
dc.description.pages29-32-
Appears in Volumess:2004: Proceeding of the workshop COST-ACTION 625 "Active fault: analysis processes and monitoring", Camerino, Italy, May 3-6 2002

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