Sfoglia per Rivista GEOLOGY
Margin architecture reveals the transition to the modern Antarctic ice sheet ca. 3 Ma
2006-01-01 Rebesco, M.; Camerlenghi, A.; Geletti, R.; Canals, M.
Margin architecture reveals the transition to the modern Antarctic ice sheet ca. 3 Ma: Reply
2007-01-01 Rebesco, M.; Camerlenghi, A.; Geletti, R.; Canals, M.
Subsurface heat and salts cause exceptionally limited methane hydrate stability in the Mediterranean Basin
2023-01-01 Camerlenghi, A.; Corradin, C.; Tinivella, U.; Giustiniani, M.; Bertoni, C.
Volcanic activities triggered or inhibited by resonance of volcanic edifices to large earthquakes
2019-01-01 Namiki, A.; Rivalta, E.; Woith, H.; Willey, T.; Parolai, S.; Walter, T. R.
Titolo | Data di pubblicazione | Autore(i) | File |
---|---|---|---|
Margin architecture reveals the transition to the modern Antarctic ice sheet ca. 3 Ma | 1-gen-2006 | Rebesco, M.; Camerlenghi, A.; Geletti, R.; Canals, M. | |
Margin architecture reveals the transition to the modern Antarctic ice sheet ca. 3 Ma: Reply | 1-gen-2007 | Rebesco, M.; Camerlenghi, A.; Geletti, R.; Canals, M. | |
Subsurface heat and salts cause exceptionally limited methane hydrate stability in the Mediterranean Basin | 1-gen-2023 | Camerlenghi, A.; Corradin, C.; Tinivella, U.; Giustiniani, M.; Bertoni, C. | |
Volcanic activities triggered or inhibited by resonance of volcanic edifices to large earthquakes | 1-gen-2019 | Namiki, A.; Rivalta, E.; Woith, H.; Willey, T.; Parolai, S.; Walter, T. R. |
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