Tertiary Tectonic Evolution of the Pannonian-Carpathian-Eastern Alpine Domain: a Personal View of from Pannonia in the Light of the Terminological Question of Tectonic Units

摘要

An abstract of an article defining boundary surfaces or zones (structural elements), and describing their geometry, characterize kinematic nature, and determining temporal evolution is presented. Results show that despite similarities of certain structural elements, the boundaries of the Miocene Alcapa unit and neotectonic "alter ego" are not the same, the southern PAF-MHZ was disintegrated and are moving with markedly different kinematics.