Mantle-derived fluids in Central Mediterranean: Geochemical and geophysical constrains on sources of fluids and migration
- Autori: CARACAUSI, A; GRASSA, F; PENNINO, V; RIZZO, A; SULLI, A
- Anno di pubblicazione: 2013
- Tipologia: eedings
- OA Link: http://hdl.handle.net/10447/83364
Abstract
The geodynamics of the central Mediterranean is
characterized by the interaction between the European plate
and the African’s. In this setting Sicily is a sector of the
Appenine-Maghrebide accretionary prism, which is located
between two areas affected by extensional tectonics (Sicily
Channel to the south and the Thyrrenian back arc basin to the
north).
Significant mantle-derived helium (0.4