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Vittorio Scribano and Serafina Carbone
Geochemical characteristics of middle ocean ridge basalts (MORBs) testify partial melting of spinel-peridotite mixed with a few amounts of garnet-pyroxenite. The latter can be considered either autochthonous products of the crystallization of partial mel...
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Claudio Argentino, Stefano Conti, Chiara Fioroni and Daniela Fontana
The occurrence of seep-carbonates associated with shallow gas hydrates is increasingly documented in modern continental margins but in fossil sediments the recognition of gas hydrates is still challenging for the lack of unequivocal proxies. Here, we com...
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Marcelo Garcia,Gerard Herail
Pág. 127 - 130
presented new and important geochronologic data on the Cenozoic magmatic rocks of northern Chile, and proposed magmatic and tectonic interpretations for them. Here we comment on one of their interpretations about the Miocene tectonic evolution of the Pre...
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Monia Calista, Francesco Mascioli, Valeria Menna, Enrico Miccadei and Tommaso Piacentini
Geomorphological evolution, erosion and retreat processes that affect the rocky coasts of the mid-western Adriatic Sea (Abruzzo, Central Italy) are the subject of this research. This coastal sector, one of the few examples of clastic soft rock coasts in ...
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Giuseppe Cianflone, Cristiano Tolomei, Carlo Alberto Brunori, Stephen Monna and Rocco Dominici
In this work, we map surficial ground deformations that occurred during the years 2004?2010 in the Crati Valley (Southern Italy). The valley is in one of the most seismically active regions of the Italian peninsula, and presents slope instability and wid...
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Giuseppe Cianflone, Cristiano Tolomei, Carlo Alberto Brunori, Stephen Monna and Rocco Dominici
In this work, we map surficial ground deformations that occurred during the years 2004?2010 in the Crati Valley (Southern Italy). The valley is in one of the most seismically active regions of the Italian peninsula, and presents slope instability and wid...
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Riccardo Bonanno, Nicola Loglisci, Silvia Cavalletto and Claudio Cassardo
Soil moisture changes are generally due to external factors (precipitation, evaporation, etc.) and internal forces (gravitational force, capillarity, transpiration, etc.). When soil temperatures remain below 0 °C for a long time (hours or even entire con...
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