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Rendiconti Online della Società Geologica Italiana - Vol. September 2010

Magmatic and metamorphic processes in late-Hercynian lower crust section from the Northern Calabria

Volume 11/2010

Eugenio Piluso (*) & Francesca Liberi (*)

Pages: 102
DOI: https://doi.org/
Rendiconti Online della Società Geologica Italiana - Vol. September 2010

Rodingites from Frido Unit: evidences for metasomatic alteration

Volume 11/2010

Maria T. Cristi Sansone (*) & Giovanna Rizzo (**)

Pages: 106-107
DOI: https://doi.org/
Rendiconti Online della Società Geologica Italiana - Vol. September 2010

Evidence for a hidden subduction-related igneous activity in the Alps during Early Eocene

Volume 11/2010

Massimo Tiepolo (*), Riccardo Tribuzio (**) & Antonio Langone (***)

Pages: 108-109
DOI: https://doi.org/
Rendiconti Online della Società Geologica Italiana - Vol. September 2010

Transient behaviour simulation of large, explosive, and ignimbrite forming eruptions by a multiphase thermo-fluid dynamic model

Volume 11/2010

Simone Lepore (*) & Claudio Scarpati (*)

Pages: 116-117
DOI: https://doi.org/
Rendiconti Online della Società Geologica Italiana - Vol. September 2010

Application of cellular automaton model for river morphological studies: CAESAR and the Pellice River (Piedmont, Italy)

Volume 11/2010

Antonio Pasculli (*), Chiara Audisio (**) & Giorgio Lollino (**)

Pages: 118-119
DOI: https://doi.org/
Rendiconti Online della Società Geologica Italiana - Vol. September 2010

An empirical-analytical mathematical model to simulate the loss in weight of Cl during the synthesis process of sodalite by the use of meta kaolinite

Volume 11/2010

Antonio Pasculli (*) & Daniela Novembre (**)

Pages: 120-121
DOI: https://doi.org/
Rendiconti Online della Società Geologica Italiana - Vol. September 2010

Application of distinct elements methods for rocky slope stability analysis in the Carrara Marble District (Apuan Alps)

Volume 11/2010

Silvia Riccucci (*), Riccardo Salvini (*), Mirko Francioni (*) & Emilio Machetti (**)

Pages: 122-123
DOI: https://doi.org/