Plio–Quaternary tectonic evolution and structure of the Catania foredeep, the northern Hyblean Plateau and the Ionian shelf (SE Sicily)
- 1 November 1998
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 298 (1-3) , 209-221
- https://doi.org/10.1016/s0040-1951(98)00185-1
Abstract
No abstract availableKeywords
This publication has 17 references indexed in Scilit:
- Early deformations at a submarine compressive front: the quaternary Catania foredeep south of Mt. Etna, Sicily, ItalyPublished by Elsevier ,2003
- The subsidence history of the northern Hyblean plateau margin, southeastern SicilyTectonophysics, 1997
- Evolution of the northwestern Iblean Mountains, Sicily: uplift, Plicocene/Pleistocene sea-level changes, paleoenvironment, and volcanismInternational Journal of Earth Sciences, 1997
- Overview of the Late Tertiary–Recent tectonic and palaeo‐environmental development of the Mediterranean regionTerra Nova, 1995
- Simulation of collision zone segmentation in the central MediterraneanTectonophysics, 1995
- Origin and role of major strike‐slip transfers during plate collision in the central MediterraneanTerra Nova, 1993
- Origin and deformation of the Neogene–Recent Maghrebian foredeep at the Gela Nappe, SE SicilyJournal of the Geological Society, 1992
- Crustal structure variations and transcurrent faulting at the eastern and western margins of the eastern MediterraneanTectonophysics, 1991
- Ionian Basin and Calabria Arc: Some new elements from DSS dataTectonophysics, 1991
- Late tortonian—lower messinian (miocene) palaeogeography of SE Sicily: information from two new formations of the sorting groupSedimentary Geology, 1982