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Italian Journal of Geosciences - Vol. February 2013

Non-marine molluscs, Upper Valdarno, central Italy, Pliocene, Pleistocene, Palaeoecology, Biochronology, Sedimentary features.

Volume 132 (2013) f.1

Daniela Esu(*) & Massimiliano Ghinassi(**)

Pages: 126-136
DOI: https://doi.org/10.3301/IJG.2012.22
Italian Journal of Geosciences - Vol. February 2013

Climate and vegetation in the Upper Valdarno Basin (central Italy) as a response to Northern Hemisphere insolation forcing and regional tectonics in the late Pliocene-early Pleistocene

Volume 132 (2013) f.1

Adele Bertini(*)

Pages: 137-148
DOI: https://doi.org/10.3301/IJG.2012.18
Italian Journal of Geosciences - Vol. February 2013

Integrating sedimentological and palaeopedological data for palaeoenvironmental reconstruction: examples from the Plio-Pleistocene Upper Valdarno Basin (Northern Apennines, Italy)

Volume 132 (2013) f.1

Francesco Fidolini(*) & Anna Andreetta(**)

Pages: 149-166
DOI: https://doi.org/10.3301/IJG.2012.26
Italian Journal of Geosciences - Vol. June 2013

Dynamics and active processes: the Albanian natural laboratory and analogues

Volume 132 (2013) f.2

François Roure(1),(2), Magdalena Scheck-Wenderoth(3), Liviu Matenco(2),Kristaq Muska(4) & Shaqir Nazai(4)

Pages: 169-174
DOI: https://doi.org/10.3301/IJG.2013.03
Italian Journal of Geosciences - Vol. June 2013

The influence of Mesozoic palaeogeography on the variations in structural style along the front of the Albanide thrust-and-fold belt

Volume 132 (2013) f.2

Andrea Argnani(*)

Pages: 175-185
DOI: https://doi.org/10.3301/IJG.2012.02
Italian Journal of Geosciences - Vol. June 2013

Focal mechanisms and slip models of moderate size earthquakes in Albania and adjacent countries

Volume 132 (2013) f.2

Anastasia Kiratzi(*) & Efthimios Dimakis

Pages: 186-193
DOI: https://doi.org/10.3301/IJG.2011.33
Italian Journal of Geosciences - Vol. June 2013

Probabilistic seismic hazard assessment in Albania

Volume 132 (2013) f.2

Betim Muço(*)

Pages: 194-202
DOI: https://doi.org/10.3301/IJG.2012.33