Erosione e sollevamento nell'arco calabro-peloritano
The Calabrian-Peloritani arc represents key site to unravel evolution of surface processes on top of subducting lithosphere. During the Pleistocene, in fact the arc uplifted at rate of the order of about 1mm/yr, forming high-standing low-relief upland (figure 2). Our study is focused on the relation...
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| Format: | Doctoral Thesis |
| Language: | it |
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Alma Mater Studiorum - Università di Bologna
2009
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| Online Access: | http://amsdottorato.unibo.it/2197/ |