Writers : Nazary, H .; shahidi, A.
Refference : The 19th Symposium on Geoscience;Tehran
Publishing Year : 1379

Abstract :
Structural belt of East Iran includes an approximately NS Continental Orogenic complex. The oldest rocks of this block relates to pre-cenomanian with due to stratigraphic and petrology example, it inferencs that there was a rifting between Iranian and Afghani continents. That causes east Iran ophiolite obducting during cretaceous era. In the same time sedimentation has occurred. There has been a Continental Environment after rifting closer in late Cretaceous. A linear magmatic . Activity has been seed. During this tectonic evolution from that time to now. Flower structures and Riedel Systems derived from a pull apart basin occur during evolution and deployment of fault systems and they make Production and propagations of different sedimentary basins.
Subject List : Tectonostratigraphy