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- W179905421 abstract "Based on a critical revision of the available structural and paleomagnetic data coupled with results from laboratory models on oceanic subduction, we suggest that the curvature of the Gibraltar Arc has been achieved throughout opposite vertical axis rotations on the two arms of the arc. Paleomagnetic rotations have been measured in the late Miocene sediments both in the Betics and in the Rif chain, providing a significant rejuvenation of the age of vertical axis rotation. Laboratory models show that the trench roll-back mechanism of a narrow subducting lithosphere can be a valuable mechanism to generate curved structures, mainly caused by toroidal return flow in the upper mantle. Such mechanism can be also extended to other Mediterranean arcs, such as the Calabrian Arc, where a clear relationship between trench-retreat and arc bending has been largely accepted. We suggest that slab roll-back pursued also after the late Miocene, but at a reduced rate and is now almost ceased. Today, the regional present-day kinematics of the western Mediterranean region is characterized by a small (~ 5 mm yr-1) west-northwest motion of the Nubia plate respect to the Eurasia plate." @default.
- W179905421 created "2016-06-24" @default.
- W179905421 creator A5010281022 @default.
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- W179905421 creator A5058067347 @default.
- W179905421 creator A5085030476 @default.
- W179905421 creator A5085764459 @default.
- W179905421 date "2007-01-01" @default.
- W179905421 modified "2023-09-28" @default.
- W179905421 title "Neogene tectonic evolution of the Betic Chain: Insights from paleomagnetic, structural analyses, and laboratory models" @default.
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