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This work reports structural and anisotropy of magnetic susceptibility (AMS) measurements from an Upper Miocene décollement level exposed in the central Apennine fold‐and‐thrust belt of Italy. The décollement level is located at the boundary between the Mesozoic‐Cenozoic carbonate sequence and the overlying Miocene‐Pliocene syn‐orogenic siliciclastic sediments and consists of a thick shear zone, mainly...
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