Scientists explain Italy's 'unzipping' crust via delamination process
Geologists led by Stefano Tavani propose that a zipper-like peeling of the lower crust explains the Apennines' paradoxical geology.
What to know
- Tavani's team proposes that delamination—a zipper-like separation of the lower crust sinking into the mantle—explains why the Apennines simultaneously compress and extend.
- The migrating delamination front, or 'hinge,' moves toward the Adriatic foreland, solving a 20+ year geological puzzle about contradictory surface movements and earthquakes.
- The process began around 2 million years ago when the major phase of extension that opened the Tyrrhenian Sea ended, yet paradoxical deformation of the mountain range continued.
Stefano Tavani Lead geologist, University of Florence
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Tavani's team proposes delamination as explanation for Apennine paradox
Geologists led by Stefano Tavani of the University of Florence present research suggesting that Earth's crust is 'unzipping' beneath Italy through a process called delamination. The lower crust and lithosphere peel away and sink into the mantle along a single migrating front—like a zipper—moving toward the Adriatic foreland, explaining why the Apennines experience both compression and extension simultaneously.
“Earth's crust is 'unzipping' under Italy, producing the strange geology on the land above. It's a process known as delamination, in which the dense lower crust and attached lithosphere peel away from the crust above and sink into the mantle.”
— ScienceAlert -
first by ScienceAlert, 13d ago
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Earth's Crust Is 'Unzipping' Under Italy https://www. sciencealert.com/earths-crust- is-unzipping-under-italy?utm_source=flipboard&utm_medium=activitypub Posted into Nature @ nature-ScienceAlert
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