Abstract
The magmatic island of Capraia in the northern Tyrrhenian Sea records late stages in the evolution of a retreating subduction zone following continental accretion. Subduction rollback in the northern Tyrrhenian Sea was accompanied by an eastward migrating magmatic arc that coincided with Capraia at ∼7.7 Ma. This was followed by segmentation of the subducting slab through eastward propagating tear faults. We present high-precision, step-heating
| Original language | English |
|---|---|
| Pages (from-to) | 30-38 |
| Journal | Journal of Geodynamics |
| Issue number | 47 |
| DOIs | |
| Publication status | Published - 2009 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 14 Life Below Water
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