The formation and growth mechanisms of young back-arc spreading ridges from high-resolution bathymetry: The Marsili Seamount (Tyrrhenian Sea, Italy)

Author:

Nicotra EugenioORCID,Passaro SalvatoreORCID,Ventura GuidoORCID

Funder

Consiglio Nazionale delle Ricerche

Publisher

Elsevier BV

Subject

General Earth and Planetary Sciences

Reference68 articles.

1. Seawater dynamics and environmental settings after November 2002 gas eruption off Bottaro (Panarea, Aeolian Islands, Mediterranean Sea);Aliani;Cont. Shelf Res.,2010

2. Geological interpretation of volcanism and segmentation of the Mariana back-arc spreading center between 12.78°N and 18.38°N;Anderson;Geochem. Geophys. Geosyst.,2017

3. Back-arc basins: A global view from geophysical synthesis and analysis;Artemieva;Earth Sci. Rev.,2023

4. Neogene to Recent volcanism of the Southern Tyrrhenian-Sicilian area: implications for the geodynamic evolution of the Calabrian Arc;Beccaluva;Earth Evolution Sciences,1982

5. Potential-field modeling of collapse-prone submarine volcanoes in the southern Tyrrhenian Sea (Italy);Caratori Tontini;Geophys. Res. Lett.,2010

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