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Using Tephrochronology and palynology to date the MIS 13 lacustrine sediments of the Mercure basin (Southern Apennines - Italy)
Volume 133 (2014) f.2
Paola Petrosino (*), Elda Russo Ermolli (*), Paola Donato (**), Brian Jicha (***), Gaetano Robustelli (**) & Raffaele Sardella (****)
Pages: 169-186
DOI: https://doi.org/10.3301/IJG.2013.22
Geoheritage and sport climbing activities: using the Montestrutto cliff (Austroalpine domain, Western Alps) as an example of scientific and educational representativeness
Volume 133 (2014) f.2
Irene Bollati (*), Michele Zucali (*), Cristina Giovenco (*) & Manuela Pelfini (*)
Pages: 187-199
DOI: https://doi.org/10.3301/IJG.2013.24
First report of Lutra simplicidens (Carnivora, Mustelidae, Lutrinae) in the Early Pleistocene of the Upper Valdarno (Italy) and the origin of European otters
Volume 133 (2014) f.2
Marco Cherin (*) & Lorenzo Rook (**)
Pages: 200-203
DOI: https://doi.org/10.3301/IJG.2013.25
An analytical model for the geotherm in the Basilicata oil fields area (southern Italy)
Volume 133 (2014) f.2
Antonella Megna (*), Stefania Candela (**), Stefano Mazzoli (***) & Stefano Santini (**)
Pages: 204-213
DOI: https://doi.org/10.3301/IJG.2014.02
The amount of pure shear and thinning in the Hercynian continental lower crust exposed in the Serre Massif (Calabria, southern Italy): an application of the vorticity analysis to quartz c-axis fabrics
Volume 133 (2014) f.2
Pages: 214-222
DOI: https://doi.org/ 10.3301/IJG.2014.03
Architecture of the western margin of the North Adriatic foreland: the Schio-Vicenza fault system
Volume 133 (2014) f.2
Marco Pola (*), Angelo Ricciato (**), Roberto Fantoni (***), Paolo Fabbri (*) & Dario Zampieri (*)
Pages: 223-234
DOI: https://doi.org/10.3301/IJG.2014.04
Land mollusc palaeocommunity dynamics related to palaeoclimatic changes in the Upper Pleistocene alluvial deposits of Marche Apennines (central Italy)
Volume 133 (2014) f.2
Carmine D’Amico (*) (**), Daniela Esu (***) & Mauro Magnatti (****)
Pages: 235-248
DOI: https://doi.org/10.3301/IJG.2014.05