
Italy's Earthquakes Linked to Crust 'Unzipping' Rather Than Plate Collision
New research indicates that seismic activity in Italy's Apennine Mountains is primarily driven by the peeling away of the lower crust into the mantle, a process known as delamination, rather than traditional plate subduction. This 'unzipping' mechanism explains the region's complex mix of compression and extension, with implications for understanding similar tectonic transitions elsewhere.






