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Fall AGU 2008 abstracts
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List of participants
List of participants (names, email addresses, affiliations) to the 2008 Calabria Summer School
Summer School 2008 Announcement
Announcement of the Summer School originally published on the Calabrian Arc website in January 2008.
Fall AGU 2008 Abstracts
Copies of seven abstracts submitted to session T03 from CAT/SCAN - Calabria Arc Project
Fall AGU 2008 abstracts
PDFs of abstracts for special session T03
Seeber et al 2008
Collision versus separation in roll-back: The Calabria Arc through the Apulia-Africa Narrow
Piana et al 2008
Crust and upper mantle seismic structure across the Calabrian Arc, Italy, from receiver function analysis
Baccheschi et al 2008
Interaction between mantle flow and slab geometry from seismic anisotropy: the Tyrrhenian Sea-Calabrian Arc subduction system
Schaefer et al 2008
Thermochronology meets cosmogenic nuclides - Comparing Pleistocene landscape denudation and catchment erosion rates
Reitz and Seeber 2008
Structural evolution of the Crotone Basin: Successive shortening and extension episodes parallel to the Calabrian Forearc (South Italy)
Dumas & Valensise 2008
Dumas, B. and Valensise, G., Recent geomorphic evolution and seismogenic processes in the Messina Straits, Field trip guide for the 2008 Calabria Summer School.
Summer school 2008 approaching
Calabria Summer School kicks off on Sunday Sept 1, 2008
Univ. of Calabria campus aerial photo
Air photo of the University of Calabria campus, showing the location of the Socrates residence and of the lecture halls of the summer school ("Cubi" 30-31).
Uplift and faulting at the transition from subduction to collision
Of the complex, retreating, stalling and foundering subduction zones of the Mediterranean, Calabria is one of the most intriguing. In contrast to the Apennines to the north and Sicily to the south, it continues to subduct oceanic lithosphere, yet convergence appears to have stalled and uplift appears to have accelerated in the Pleistocene. Modern uplift rates are some of the highest in the Adriatic subduction systems. This project focuses an array of modern analysis techniques on this problem: first, by refining the observations of horizontal and vertical motions back through time and second, by linking these to geodynamic models of upper mantle, lithospheric and crustal deformation.