History of subduction and back-arc extension in the Central Mediterranean

Details History of subduction and back-arc extension in the Central Mediterranean History of subduction and back-arc extension in the Central Mediterranean

Jun 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001geoji.145..809f&link_type=abstract

Geophysical Journal International, Volume 145, Issue 3, pp. 809-820.

Astronomy and Astrophysics

Astronomy

97

Back-Arc Extension, Mantle Convection, Mediterranean, Subduction, Tectonics, Tomography

Scientific paper

Geological and geophysical constraints to reconstruct the evolution of the Central Mediterranean subduction zone are presented. Geological observations such as upper plate stratigraphy, HP-LT metamorphic assemblages, foredeep/trench stratigraphy, arc volcanism and the back-arc extension process are used to define the infant stage of the subduction zone and its latest, back-arc phase. Based on this data set, the time dependence of the amount of subducted material in comparison with the tomographic images of the upper mantle along two cross-sections from the northern Apennines and from Calabria to the Gulf of Lyon can be derived. Further, the reconstruction is used to unravel the main evolutionary trends of the subduction process. Results of this analysis indicate that (1) subduction in the Central Mediterranean is as old as 80Myr, (2) the slab descended slowly into the mantle during the first 20-30Myr (subduction speeds were probably less than 1cmyear-1), (3) subduction accelerated afterwards, producing arc volcanism and back-arc extension and (4) the slab reached the 660km transition zone after 60-70Myr. This time-dependent scenario, where a slow initiation is followed by a roughly exponential increase in the subduction speed, can be modelled by equating the viscous dissipation per unit length due to the bending of oceanic lithosphere to the rate of change of potential energy by slab pull. Finally, the third stage is controlled by the interaction between the slab and the 660km transition zone. In the southern region, this results in an important re-shaping of the slab and intermittent pulses of back-arc extension. In the northern region, the decrease in the trench retreat can be explained by the entrance of light continental material at the trench.

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