Please use this identifier to cite or link to this item: http://dx.doi.org/10.15165/studgeocam-1430
Title: DEFORMAZIONI DA TAGLIO IN MATERIALI ARGILLOSI: ANALISI DEI SEDIMENTI DEFORMATI DALLA FAGLIA DI SCORCIABUOI
Other Titles: Shear deformation in pelitic materials: Analysis of sediments deformed by the Scorciabuoi fault
Authors: CASCIELLO, E.
Keywords: deformazioni da taglio - faglia trascorrente - materiali argillosi - illite/smectite - Appennino meridionale
shear deformation - strike-slip fault - argillaceous materials - illite/smectite - Southem Apennines
Issue Date: 2002
Publisher: Università di Camerino
Citation: Studi geologici camerti. Nuova serie, 2002/1, pp.51-62
Abstract: In this work the macro-structural features and the fabric of a regional strike-slip fault, exposed in the southern Apennines and known as the Scorciabuoi fault, are described. On a regional scale the Scorciabuoi fault is a N 115° trending discontinuity cutting obliquely the frontal portions of the Southern Apennines fold-and­thrust-belt (CARBONE et alii, 1991, CELLO & MAZZOLI, 1999; PATACCA & SCANDONE, 1999; CASCIELLO, 1999; BON!Nl & SANI, 2000). The fault piane, exposed in different localities, displays a clear left-transtensional displacement with lineation pitch ranging between 35° east and sub-horizontal. [...]
URI: http://193.204.8.201:8080/jspui/handle/1336/809
ISSN: 1827-1979
Appears in Volumess:Volume 2002/1

Files in This Item:
File SizeFormat 
Vol. 2002-1 Capitolo 4 p.51.pdf
Restricted Access
1,63 MBAdobe PDFView/Open Ask to the Librarian


This item is protected by original copyright



Items in Archive are protected by copyright, with all rights reserved, unless otherwise indicated.