Veiskarami, Marzieh

[ 1 ] - Majerad gabrodorites in the southeast of Shahrood: An evidence to the starting of opening of the supra-subduction basin of the Sabzevar Neotethyian branch in the middle Jurassic

Late Neoproterozoic Majerad basementic igneous - metamorphic complex with NE-SW trend located in the 150 Km southeast Shahrood and north edge of the central Iran structural zone. Same as the other basementic complex of southeast of Shahroud, in the north of Majerad pass, this complex crosscut by several small scale gabrrodioritic intrusions and numerous diabasic dikes. In these gabrodiorite int...