New SKS data consistent with previously defined mantle deformation patterns
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Geodynamic model for Central Mediterranean from new seismic anisotropy data
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NW-SE Apenninic mantle anisotropy interrupted by a narrow well developed mantle flow
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Seismic anisotropy consistent with shallow horizontal slab tear beneath central Italy
Abstract
In the middle of the Mediterranean, the partly still active Apennines subduction system has been usually defined using tomographic images and available shear wave splitting measurements. In this paper we describe the new seismic anisotropy dataset for Central Italy, the region where the transition between Northern and Southern Apennines occurs. The new measurements show NW-SE fast polarisation directions beneath the belt, due to the retreat of the slab, NNE-SSW orientations from proper Adriatic mantle sources, and E-W directed anisotropy, attributed to mantle convection flow at the Thyrranian side. Additionally, the new data suggest the presence of a toroidal mantle flow through a tear in the Apenninic slab, from the Adria to the Tyrrhenian side. However, mantle circulation and flows, identified by the pattern of shear wave splitting results, seem different from what was proposed in previous geodynamic models. Indeed, our results support the presence of a vertical slab tear with limited dimension. In the geodynamic model we propose, the tear acts to accommodate a differential slab retreat. The slab partitioning results in a different pattern and strength of seismic anisotropy traced from the Central Apennines with respect to the adjacent Northern and Southern Apennines.
Keywords
Seismic anisotropy
Mantle flows
Geodynamic model
Apennines
Central Mediterranean
Data availability
Alla data used are available and described along with the paper.