Tectonic and Stratigraphic Evolution of Zagros and Makran During the Mesozoic-Cenozoic

The Zagros fold-thrust belt (ZFTB) extends from Turkey to the Hormuz Strait, resulting from the collision of the Arabian and Eurasian plates during Cenozoic times, and separates the Arabian platform from the large plateaux of central Iran. In this volume the structure of the Zagros Mountains is explored through different scales and using different methodologies.