Analysis reveals subduction-related paleostress and deformation temperatures in the Sestola-Vidiciatico unit, suggesting complex geological processes in the Northern Apennines.
Supplemental material includes stereoplots of the various described structures, stress inversion tensor averaging, and outcrop photo of anastamosing foliation and thrust faults at the Riolunato site.
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Williams et al. (2025) studied this question.
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