Miocene‐Pliocene tectonic evolution of the Slovenian Periadriatic fault: Implications for Alpine‐Carpathian extrusion models

The Periadriatic Line (PAL) is a remarkable, several hundred kilometer long fault system of the Alpine orogen. Its dextral character was documented by several authors using diverse criteria, but detailed kinematics and timing of movements had not been investigated along its whole length. Structural ... View More