Tectonically-driven mud volcanism since the late Pliocene on the Calabrian accretionary prism, central Mediterranean Sea

Author:

Praeg D.,Ceramicola S.,Barbieri R.,Unnithan V.,Wardell N.

Publisher

Elsevier BV

Subject

Stratigraphy,Economic Geology,Geology,Geophysics,Oceanography

Reference81 articles.

1. Sedimentary succession and evolution of the Mediterranean Ridge western sector as derived from lithology of mud breccia clasts;Akhmanov;Marine Geology,2003

2. Dati geologici preliminary sul bacino di Crotone-Spartivento (Mar Ionio);Barbieri;Acta Naturalia de l'Ateneo Parmense,1982

3. Geological structure and evolution of the marine areas adjacent to the Calabrian Arc;Barone;Earth Evolution Sciences,1982

4. The Calabrian arc and the Ionian sea in the dynamic evolution of the central Mediterranean;Boccaletti;Marine Geology,1984

5. Interrelations of mud volcanism, fluid venting, and thrust-anticline folding: examples from the external northern Apennines (Emilia-Romagna, Italy);Bonini;Journal of Geophysical Research,2007

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